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description Publicationkeyboard_double_arrow_right Part of book or chapter of book 2016 FrancePublisher:Integrated Ocean Drilling Program Authors: Deans, Jeremy; ILDEFONSE, Benoit;Deans, Jeremy; ILDEFONSE, Benoit;Ocean Drilling Program (ODP) Hole 1256D is the first in situ penetration into the sheeted dike/gabbro transition zone and was drilled over the course of several expeditions. The hole was initiated during ODP Leg 206 and lengthened during Integrated Ocean Drilling Program Expeditions 309, 312, and 335. Nine samples were analyzed from two gabbroic sections (Gabbros 1 and 2) recovered from Expedition 312 for crystallographic-preferred orientation of plagioclase, clinopyroxene, olivine, and orthopyroxene. Plagioclase and clinopyroxene are the focus of this study because these two phases are the most modally abundant minerals. Our results are compared with shape-preferred orientations from the same samples. The results demonstrate the absence of crystallographic-preferred orientation in any phases analyzed. Even though the nature of the sheeted dike/gabbro transition zone is still poorly constrained, our results are similar to those reported in rocks that have been interpreted to represent the crystallized axial melt lens in the Oman ophiolite.
https://doi.org/10.2... arrow_drop_down https://doi.org/10.2204/iodp.p...Part of book or chapter of book . 2016 . Peer-reviewedLicense: CC BYData sources: CrossrefMémoires en Sciences de l'Information et de la CommunicationPart of book or chapter of book . 2016add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.2204/iodp.proc.335.204.2016&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routeshybrid 0 citations 0 popularity Average influence Average impulse Average Powered by BIP!more_vert https://doi.org/10.2... arrow_drop_down https://doi.org/10.2204/iodp.p...Part of book or chapter of book . 2016 . Peer-reviewedLicense: CC BYData sources: CrossrefMémoires en Sciences de l'Information et de la CommunicationPart of book or chapter of book . 2016add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.2204/iodp.proc.335.204.2016&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book 2019 FrancePublisher:Springer International Publishing Marco Taviani; Agostina Vertino; Lorenzo Angeletti; Paolo Montagna; Alessandro Remia;Atlantic-type scleractinian cold-water corals occur in the Quaternary of the Mediterranean basin. Most fossil evidence on-land is Early Pleistocene in age, and occurs in peninsular Italy, Sicily and on some Greek islands, whilst submerged situations are by large late Pleistocene. According to circumstances, the mode of preservation of fossil cold-water coral varies sensibly (from loose corals to micritic limestones) what affects the level of confidence of the paleoecological reconstruction. All known situations point about a bathyal setting for such cold-water coral hosting deposits in the Mediterranean basin, but under many respects the geological record of cold-water coral paleoenvironments is yet largely underworked. Research developments are discussed, with special emphasis on the widespread submarine occurrences which prevail over the on-land cold-water coral legacy.
https://doi.org/10.1... arrow_drop_down https://doi.org/10.1007/978-3-...Part of book or chapter of book . 2019 . Peer-reviewedLicense: Springer TDMData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/978-3-319-91608-8_2&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu4 citations 4 popularity Top 10% influence Average impulse Average Powered by BIP!more_vert https://doi.org/10.1... arrow_drop_down https://doi.org/10.1007/978-3-...Part of book or chapter of book . 2019 . Peer-reviewedLicense: Springer TDMData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/978-3-319-91608-8_2&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Preprint , Conference object , Article , Part of book or chapter of book 2020 France, France, United StatesPublisher:SPIE Funded by:NSF | Collaborative Research: I..., NSF | Collaborative Research: I..., NSF | Collaborative Research: B... +5 projectsNSF| Collaborative Research: Imaging the Beginning of Time from the South Pole: Observations with the Full SPUD Array ,NSF| Collaborative Research: Imaging the Beginning of Time from the South Pole: Observations with the Full SPUD Array ,NSF| Collaborative Research: BICEP2 and SPUD - A Search for Inflation with Degree-Scale Polarimetry from the South Pole ,NSF| Collaborative Research: BICEP2 and SPUD - A Search for Inflation with Degree-Scale Polarimetry from the South Pole ,NSF| Collaborative Research: BICEP2 and SPUD - A Search for Inflation with Degree-Scale Polarimetry from the South Pole ,NSF| MRI: Development of a 150 GHz Receiver for the BICEP Array CMB Polarimeter ,NSF| Collaborative Research: Imaging the Beginning of Time from the South Pole: Observations with the Full SPUD Array ,NSF| Collaborative Research: BICEP2 and SPUD - A Search for Inflation with Degree-Scale Polarimetry from the South PoleJ. Kang; P. A. R. Ade; Zeeshan Ahmed; Mandana Amiri; Denis Barkats; R. Basu Thakur; Colin A. Bischoff; James J. Bock; H. Boenish; E. Bullock; Victor Buza; J. Cheshire; Jake Connors; J. Cornelison; M. Crumrine; A. Cukierman; E. V. Denison; Marion Dierickx; Lionel Duband; M. Eiben; S. Fatigoni; Jeffrey P. Filippini; S. Fliescher; Neil Goeckner-Wald; D. C. Goldfinger; J. A. Grayson; Paul K. Grimes; G. Hall; Mark Halpern; Sarah M. Harrison; S. Henderson; Sergi R. Hildebrandt; Gene C. Hilton; Johannes Hubmayr; Howard Hui; Kent D. Irwin; Kirit Karkare; E. Karpel; S. Kefeli; S. A. Kernasovskiy; John M Kovac; Chao-Lin Kuo; King Tong Lau; E. M. Leitch; K. G. Megerian; L. Minutolo; Lorenzo Moncelsi; Y. Nakato; Toshiya Namikawa; H. T. Nguyen; Roger O'Brient; R. W. Ogburn; S. Palladino; N. Precup; T. Prouve; C. Pryke; B. Racine; Carl D. Reintsema; S. Richter; Alessandro Schillaci; Benjamin L. Schmitt; R. Schwarz; C. D. Sheehy; Ahmed Soliman; T. St. Germaine; Bryan Steinbach; Rashmikant V. Sudiwala; G. P. Teply; Keith L. Thompson; J. E. Tolan; Carole Tucker; Anthony D. Turner; C. Umiltà; Abigail G. Vieregg; A. Wandui; A. C. Weber; Donald V. Wiebe; J. Willmert; C. L. Wong; W. L. K. Wu; Eui-Hyeok Yang; Ki Won Yoon; Edward D. Young; Che-Hang Yu; Lingzhen Zeng; Chao Zhang; Shengyu Zhang;BICEP3 is a 520 mm aperture on-axis refracting telescope at the South Pole, which observes the polarization of the cosmic microwave background (CMB) at 95 GHz to search for the B-mode signal from inflationary gravitational waves. In addition to this main target, we have developed a low-elevation observation strategy to extend coverage of the Southern sky at the South Pole, where BICEP3 can quickly achieve degree-scale E-mode measurements over a large area. An interesting E-mode measurement is probing a potential polarization anomaly around the CMB Cold Spot. During the austral summer seasons of 2018-19 and 2019-20, BICEP3 observed the sky with a flat mirror to redirect the beams to various low elevation ranges. The preliminary data analysis shows degree-scale E-modes measured with high signal-to-noise ratio. Comment: 12 pages, 10 figures; Figure 7 shows the correct file
Caltech Authors arrow_drop_down Mémoires en Sciences de l'Information et de la Communication; HAL-CEAConference object . 2020https://doi.org/10.48550/arxiv...Article . 2020License: arXiv Non-Exclusive DistributionData sources: Dataciteadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1117/12.2562066&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen 1 citations 1 popularity Average influence Average impulse Average Powered by BIP!more_vert Caltech Authors arrow_drop_down Mémoires en Sciences de l'Information et de la Communication; HAL-CEAConference object . 2020https://doi.org/10.48550/arxiv...Article . 2020License: arXiv Non-Exclusive DistributionData sources: Dataciteadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1117/12.2562066&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book 2015 FrancePublisher:Springer Netherlands Renate Forkel; Alex Guenther; Kirsti Ashworth; Carole Bedos; Claire Delon; J. Lathière; Steffen M. Noe; Elise Potier; Janne Rinne; O. Tchepel; Leiming Zhang;International audience; Volatile organic compounds (VOC) are a relatively minor component of the atmosphere and yet are widely recognized to have important roles in air quality and climate. With the exception of methane, an important greenhouse gas, atmospheric VOC are primarily of interest because of their impact on other atmospheric constituents, including oxidants and aerosol.
https://doi.org/10.1... arrow_drop_down https://doi.org/10.1007/978-94...Part of book or chapter of book . 2015 . Peer-reviewedData sources: CrossrefMémoires en Sciences de l'Information et de la Communication; HAL-CEA; Hal-DiderotPart of book or chapter of book . 2015License: CC BY NCadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/978-94-017-7285-3_8&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu2 citations 2 popularity Average influence Average impulse Average Powered by BIP!more_vert https://doi.org/10.1... arrow_drop_down https://doi.org/10.1007/978-94...Part of book or chapter of book . 2015 . Peer-reviewedData sources: CrossrefMémoires en Sciences de l'Information et de la Communication; HAL-CEA; Hal-DiderotPart of book or chapter of book . 2015License: CC BY NCadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/978-94-017-7285-3_8&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book 2013 FrancePublisher:American Geophysical Union (AGU) Authors: Hirth, Greg; Escartin, Javier; Lin, Jian;Hirth, Greg; Escartin, Javier; Lin, Jian;doi: 10.1029/gm106p0291
An analysis of experimentally determined flow laws for gabbroic rocks indicates that the lower oceanic crust is considerably stronger than commonly assumed in many modeling studies. A combination of experimental, geochemical and petrological constraints suggest that the majority of the lower oceanic crust is almost dry prior to hydrothermal alteration. Several geological and geophysical observations also indicate that the strength of the lower ocean crust approaches that of dry gabbroic rock. These observations are inconsistent with commonly used rheological models for the oceanic lithosphere that incorporate a weak lower crust that decouples a strong upper mantle from a brittle upper crust.
Hal-Diderot arrow_drop_down Mémoires en Sciences de l'Information et de la CommunicationPart of book or chapter of book . 2013https://doi.org/10.1029/gm106p...Part of book or chapter of book . 2013 . Peer-reviewedData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1029/gm106p0291&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu74 citations 74 popularity Top 10% influence Top 10% impulse Top 1% Powered by BIP!more_vert Hal-Diderot arrow_drop_down Mémoires en Sciences de l'Information et de la CommunicationPart of book or chapter of book . 2013https://doi.org/10.1029/gm106p...Part of book or chapter of book . 2013 . Peer-reviewedData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1029/gm106p0291&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book , Other literature type 2020 FrancePublisher:Springer International Publishing Authors: Denis-Didier Rousseau; Christine Hatté;Denis-Didier Rousseau; Christine Hatté;Atmospheric circulation is responsible for the rapid distribution of heat and moisture across the Earth and hence determines our weather and regional climate, today and in the past. During past climate cycles, the atmosphere has been much more dustier, except during the interglacials, inducing uncertainties about the impact of mineral aerosols on the past climate dynamics. There are abundant traces of the combination of past atmospheric dynamics and paleodust cycle such as eolian mineral material transported and deposited in terrestrial archives as loess. Records from loess deposits consistently suggest that atmospheric dynamics was highly variable, during the past climate cycles, much more than presently where the only sources of dust are the major deserts. In this chapter we explained the four main categories of parameters allowing to identify loess deposits as reliable markers for past air circulation. Open image in new window Fig. 13.1 Global distribution of loess sediments and equivalents. 1: loess sediments; 2: loess derivatives (according to Pecsi (1990))
https://academiccomm... arrow_drop_down https://doi.org/10.1007/978-3-...Part of book or chapter of book . 2020 . Peer-reviewedLicense: Springer TDMData sources: CrossrefMémoires en Sciences de l'Information et de la Communication; HAL-CEAPart of book or chapter of book . 2021add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/978-3-030-24982-3_13&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu2 citations 2 popularity Average influence Average impulse Average Powered by BIP!more_vert https://academiccomm... arrow_drop_down https://doi.org/10.1007/978-3-...Part of book or chapter of book . 2020 . Peer-reviewedLicense: Springer TDMData sources: CrossrefMémoires en Sciences de l'Information et de la Communication; HAL-CEAPart of book or chapter of book . 2021add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/978-3-030-24982-3_13&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book 2013 FrancePublisher:Springer Netherlands Authors: Angielczyk, Kenneth, D; Steyer, Jean-Sébastien; Sidor, Christian, A; Smith, Roger; +2 AuthorsAngielczyk, Kenneth, D; Steyer, Jean-Sébastien; Sidor, Christian, A; Smith, Roger; Whatley, Robin, L; Tolan, Stephen;Dicynodont fossils were first collected in the Luangwa Basin, Zambia, in the 1920s, but limited detailed study and taxonomic uncertainty have obscured their biostratigraphic utility and their implications for topics such as dicynodont biogeography and the effects of the end-Permian extinction. Here we present a comprehensive taxonomic revision of the dicynodonts of the Luangwa Basin, taking into account specimens in all major museum collections and new material collected by our team in 2009. We recognize 14 dicynodont species from the Upper Permian Upper Madumabisa Mudstone: Pristerodon mackayi, Endothiodon sp., Diictodon feliceps, Compsodon helmoedi, Emydops sp., Dicynodontoides cf. D. nowacki, a new tusked cistecephalid, cf. Katumbia parringtoni, Kitchinganomodon crassus, Oudenodon bainii, Odontocyclops whaitsi, Dicynodon huenei, Syops vanhoepeni, and a new lystrosaurid. Previous reports of Lystrosaurus in the basin appear to be in error. In addition, we found no significant partitioning of dicynodont taxa in the northern and southern parts of the basin, despite substantial differences in preservation, indicating the presence of a single faunal assemblage in the Upper Permian. The Madumabisa dicynodont assemblage is best correlated with the Cistecephalus Assemblage Zone of South Africa. The shared presence of Dicynodon huenei and possibly Katumbia in the Luangwa Basin and the Ruhuhu Basin of Tanzania suggests that the Tanzanian Usili Formation also can be correlated with the Cistecephalus zone. Interestingly, the Madumabisa assemblage from Zambia is more similar to the coeval assemblage from South Africa, despite its closer geographic proximity to Tanzania. The Karoo and Ruhuhu basins also include more endemic species in the Permian than the Luangwa Basin. The Middle Triassic Ntawere Formation preserves four dicynodont species (Kannemeyeria lophorhinus, “Kannemeyeria” latirostris, Zambiasaurus submersus, Sangusaurus edentatus), which occur at two stratigraphic levels. The lower Ntawere assemblage resembles that of the Omingonde Formation of Namibia in the presence of Kannemeyeria lophorhinus and potentially Dolichuranus (if “K.” latirostris represents this taxon). The upper Ntawere assemblage shares the genus Sangusaurus with that of the Manda beds of Tanzania and includes the endemic Zambiasaurus. Comparisons of these assemblages to the Omingonde and Manda suggest that both are best correlated with the Cynognathus C subzone. When combined with data on other tetrapod taxa, our revised dicynodont assemblages contribute to an emerging picture of broad faunal similarity in southern and eastern Africa during the Late Permian, and increasing differentiation between the South African and other Karoo basins following the end-Permian extinction.
https://doi.org/10.1... arrow_drop_down https://doi.org/10.1007/978-94...Part of book or chapter of book . 2013 . Peer-reviewedLicense: Springer Nature TDMData sources: CrossrefMémoires en Sciences de l'Information et de la Communication; HAL-UPMCPart of book or chapter of book . 2014Full-Text: https://hal.science/hal-02107892/documentMémoires en Sciences de l'Information et de la Communication; Hal-DiderotPart of book or chapter of book . 2014add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/978-94-007-6841-3_7&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu71 citations 71 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!more_vert https://doi.org/10.1... arrow_drop_down https://doi.org/10.1007/978-94...Part of book or chapter of book . 2013 . Peer-reviewedLicense: Springer Nature TDMData sources: CrossrefMémoires en Sciences de l'Information et de la Communication; HAL-UPMCPart of book or chapter of book . 2014Full-Text: https://hal.science/hal-02107892/documentMémoires en Sciences de l'Information et de la Communication; Hal-DiderotPart of book or chapter of book . 2014add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/978-94-007-6841-3_7&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Part of book or chapter of book , Other literature type 2013 FrancePublisher:Springer International Publishing Praeg, D.; Ketzer, J.Marcelo; Augustin, A.H.; Migeon, S.; Ceramicola, S.; Dano, A.; Ducassou, E.; Dupré, S.; Mascle, J.; Rodrigues, L. F.;International audience; On the central Nile deep-sea fan, stratified sediments overlying mass-transport deposits (MTDs) are deformed into slope-parallel seabed undulations associated with fluid seepage. The western part of this system, in water depths of 1,950-2,250 m, is examined using multi-frequency data from hull-mounted and deep-towed swath/profiling systems. Sub-bottom profiles show sub-vertical fluid pipes that terminate both at and below seabed, and gas signatures along fault planes bounding the undulations. Fluid seepage is recorded by high- to intermediate-backscatter patches (HBPs, IBPs) that differ in appearance on multibeam imagery (30 kHz, ≤3 m penetration) and sidescan swaths (170/190 kHz, <0.1 m penetration). Comparison of the two suggests a distinction of (a) buried carbonates (0.1-3 m), (b) broad near-seabed (<0.1 m) carbonate pavements elongate along the undulations, (c) sub-circular areas of seabed seepage up to 300 m across. Four of the latter have narrower gas flares at their edges rising 400-800 m above seabed. These results are consistent with an evolving system of narrow fluid conduits that support the growth and burial of carbonate pavements, shifting over millennial timescales along linear zones parallel to fault planes rooted in MTDs. Sediment deformation above MTDs is inferred to provide pathways for fluid escape, but migration of gas-rich fluids from depth is likely to have facilitated slope destabilisation
https://archimer.ifr... arrow_drop_down ArchiMer - Institutional Archive of IfremerOther literature type . 2014Data sources: ArchiMer - Institutional Archive of Ifremerhttps://doi.org/10.1007/978-3-...Part of book or chapter of book . 2013 . Peer-reviewedLicense: Springer Nature TDMData sources: CrossrefHAL - UPEC / UPEM; HAL-Inserm; Hal-DiderotArticle . 2014add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/978-3-319-00972-8_13&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu11 citations 11 popularity Average influence Average impulse Top 10% Powered by BIP!visibility 7visibility views 7 Powered bymore_vert https://archimer.ifr... arrow_drop_down ArchiMer - Institutional Archive of IfremerOther literature type . 2014Data sources: ArchiMer - Institutional Archive of Ifremerhttps://doi.org/10.1007/978-3-...Part of book or chapter of book . 2013 . Peer-reviewedLicense: Springer Nature TDMData sources: CrossrefHAL - UPEC / UPEM; HAL-Inserm; Hal-DiderotArticle . 2014add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/978-3-319-00972-8_13&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book 2020 FrancePublisher:International Ocean Discovery Program Funded by:ANR | HimalFanANR| HimalFanSebastien Jean Paul Lenard; J. W. Cruz; Christian France-Lanord; Jérôme Lavé; Brendan T Reilly;International audience
https://doi.org/10.1... arrow_drop_down https://doi.org/10.14379/iodp....Part of book or chapter of book . 2020 . Peer-reviewedLicense: CC BYData sources: Crossrefhttps://hal.univ-lorraine.fr/h...Part of book or chapter of bookLicense: CC BYData sources: UnpayWallMémoires en Sciences de l'Information et de la Communication; Hal-DiderotPart of book or chapter of book . 2020add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.14379/iodp.proc.354.203.2020&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routeshybrid 6 citations 6 popularity Top 10% influence Average impulse Top 10% Powered by BIP!more_vert https://doi.org/10.1... arrow_drop_down https://doi.org/10.14379/iodp....Part of book or chapter of book . 2020 . Peer-reviewedLicense: CC BYData sources: Crossrefhttps://hal.univ-lorraine.fr/h...Part of book or chapter of bookLicense: CC BYData sources: UnpayWallMémoires en Sciences de l'Information et de la Communication; Hal-DiderotPart of book or chapter of book . 2020add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.14379/iodp.proc.354.203.2020&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Other literature type , Part of book or chapter of book , Article , Preprint 2013 France, United KingdomPublisher:Springer Netherlands Publicly fundedFunded by:EC | ECLAIRE, EC | PEGASOSEC| ECLAIRE ,EC| PEGASOSChristophe Flechard; Raia Silvia Massad; Benjamin Loubet; Erwan Personne; David Simpson; Jesse O. Bash; Ellen J. Cooter; Eiko Nemitz; Mark A. Sutton;Atmospheric ammonia (NH3) dominates global emissions of total reactive nitrogen (Nr), while emissions from agricultural production systems contribute about two-thirds of global NH3 emissions; the remaining third emanates from oceans, natural vegetation, humans, wild animals and biomass burning. On land, NH3 emitted from the various sources eventually returns to the biosphere by dry deposition to sink areas, predominantly semi-natural vegetation, and by wet and dry deposition as ammonium (NH4+) to all surfaces. However, the land/atmosphere exchange of gaseous NH3 is in fact bi-directional over unfertilized as well as fertilized ecosystems, with periods and areas of emission and deposition alternating in time (diurnal, seasonal) and space (patchwork landscapes). The exchange is controlled by a range of environmental factors, including meteorology, surface layer turbulence, thermodynamics, air and surface heterogeneous-phase chemistry, canopy geometry, plant development stage, leaf age, organic matter decomposition, soil microbial turnover, and, in agricultural systems, by fertilizer application rate, fertilizer type, soil type, crop type, and agricultural management practices. We review the range of processes controlling NH3 emission and uptake in the different parts of the soil-canopy-atmosphere continuum, with NH3 emission potentials defined at the substrate and leaf levels by different [NH4+] / [H+] ratios (Γ). Surface/atmosphere exchange models for NH3 are necessary to compute the temporal and spatial patterns of emissions and deposition at the soil, plant, field, landscape, regional and global scales, in order to assess the multiple environmental impacts of airborne and deposited NH3 and NH4+. Models of soil/vegetation/atmosphere NH3 exchange are reviewed from the substrate and leaf scales to the global scale. They range from simple steady-state, "big leaf" canopy resistance models, to dynamic, multi-layer, multi-process, multi-chemical species schemes. Their level of complexity depends on their purpose, the spatial scale at which they are applied, the current level of parameterization, and the availability of the input data they require. State-of-the-art solutions for determining the emission/sink Γ potentials through the soil/canopy system include coupled, interactive chemical transport models (CTM) and soil/ecosystem modelling at the regional scale. However, it remains a matter for debate to what extent realistic options for future regional and global models should be based on process-based mechanistic versus empirical and regression-type models. Further discussion is needed on the extent and timescale by which new approaches can be used, such as integration with ecosystem models and satellite observations.
Biogeosciences; NERC... arrow_drop_down Biogeosciences; NERC Open Research ArchiveArticle . 2013 . Peer-reviewedhttps://doi.org/10.1007/978-94...Part of book or chapter of book . 2013 . Peer-reviewedLicense: CC BY NCMémoires en Sciences de l'Information et de la CommunicationArticle . 2013Full-Text: https://hal.science/hal-01190540/documentHAL - UPEC / UPEM; HAL-Pasteur; HAL-Inserm; Hal-DiderotArticle . 2013Mémoires en Sciences de l'Information et de la CommunicationPart of book or chapter of book . 2015HAL - UPEC / UPEM; HAL-Pasteur; HAL-Inserm; Hal-DiderotPart of book or chapter of book . 2015add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/978-94-017-7285-3_2&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routesgold 108 citations 108 popularity Top 10% influence Top 10% impulse Top 1% Powered by BIP!visibility 3visibility views 3 download downloads 35 Powered bymore_vert Biogeosciences; NERC... arrow_drop_down Biogeosciences; NERC Open Research ArchiveArticle . 2013 . Peer-reviewedhttps://doi.org/10.1007/978-94...Part of book or chapter of book . 2013 . Peer-reviewedLicense: CC BY NCMémoires en Sciences de l'Information et de la CommunicationArticle . 2013Full-Text: https://hal.science/hal-01190540/documentHAL - UPEC / UPEM; HAL-Pasteur; HAL-Inserm; Hal-DiderotArticle . 2013Mémoires en Sciences de l'Information et de la CommunicationPart of book or chapter of book . 2015HAL - UPEC / UPEM; HAL-Pasteur; HAL-Inserm; Hal-DiderotPart of book or chapter of book . 2015add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/978-94-017-7285-3_2&type=result"></script>'); --> </script>
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description Publicationkeyboard_double_arrow_right Part of book or chapter of book 2016 FrancePublisher:Integrated Ocean Drilling Program Authors: Deans, Jeremy; ILDEFONSE, Benoit;Deans, Jeremy; ILDEFONSE, Benoit;Ocean Drilling Program (ODP) Hole 1256D is the first in situ penetration into the sheeted dike/gabbro transition zone and was drilled over the course of several expeditions. The hole was initiated during ODP Leg 206 and lengthened during Integrated Ocean Drilling Program Expeditions 309, 312, and 335. Nine samples were analyzed from two gabbroic sections (Gabbros 1 and 2) recovered from Expedition 312 for crystallographic-preferred orientation of plagioclase, clinopyroxene, olivine, and orthopyroxene. Plagioclase and clinopyroxene are the focus of this study because these two phases are the most modally abundant minerals. Our results are compared with shape-preferred orientations from the same samples. The results demonstrate the absence of crystallographic-preferred orientation in any phases analyzed. Even though the nature of the sheeted dike/gabbro transition zone is still poorly constrained, our results are similar to those reported in rocks that have been interpreted to represent the crystallized axial melt lens in the Oman ophiolite.
https://doi.org/10.2... arrow_drop_down https://doi.org/10.2204/iodp.p...Part of book or chapter of book . 2016 . Peer-reviewedLicense: CC BYData sources: CrossrefMémoires en Sciences de l'Information et de la CommunicationPart of book or chapter of book . 2016add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.2204/iodp.proc.335.204.2016&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routeshybrid 0 citations 0 popularity Average influence Average impulse Average Powered by BIP!more_vert https://doi.org/10.2... arrow_drop_down https://doi.org/10.2204/iodp.p...Part of book or chapter of book . 2016 . Peer-reviewedLicense: CC BYData sources: CrossrefMémoires en Sciences de l'Information et de la CommunicationPart of book or chapter of book . 2016add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.2204/iodp.proc.335.204.2016&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book 2019 FrancePublisher:Springer International Publishing Marco Taviani; Agostina Vertino; Lorenzo Angeletti; Paolo Montagna; Alessandro Remia;Atlantic-type scleractinian cold-water corals occur in the Quaternary of the Mediterranean basin. Most fossil evidence on-land is Early Pleistocene in age, and occurs in peninsular Italy, Sicily and on some Greek islands, whilst submerged situations are by large late Pleistocene. According to circumstances, the mode of preservation of fossil cold-water coral varies sensibly (from loose corals to micritic limestones) what affects the level of confidence of the paleoecological reconstruction. All known situations point about a bathyal setting for such cold-water coral hosting deposits in the Mediterranean basin, but under many respects the geological record of cold-water coral paleoenvironments is yet largely underworked. Research developments are discussed, with special emphasis on the widespread submarine occurrences which prevail over the on-land cold-water coral legacy.
https://doi.org/10.1... arrow_drop_down https://doi.org/10.1007/978-3-...Part of book or chapter of book . 2019 . Peer-reviewedLicense: Springer TDMData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/978-3-319-91608-8_2&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu4 citations 4 popularity Top 10% influence Average impulse Average Powered by BIP!more_vert https://doi.org/10.1... arrow_drop_down https://doi.org/10.1007/978-3-...Part of book or chapter of book . 2019 . Peer-reviewedLicense: Springer TDMData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/978-3-319-91608-8_2&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Preprint , Conference object , Article , Part of book or chapter of book 2020 France, France, United StatesPublisher:SPIE Funded by:NSF | Collaborative Research: I..., NSF | Collaborative Research: I..., NSF | Collaborative Research: B... +5 projectsNSF| Collaborative Research: Imaging the Beginning of Time from the South Pole: Observations with the Full SPUD Array ,NSF| Collaborative Research: Imaging the Beginning of Time from the South Pole: Observations with the Full SPUD Array ,NSF| Collaborative Research: BICEP2 and SPUD - A Search for Inflation with Degree-Scale Polarimetry from the South Pole ,NSF| Collaborative Research: BICEP2 and SPUD - A Search for Inflation with Degree-Scale Polarimetry from the South Pole ,NSF| Collaborative Research: BICEP2 and SPUD - A Search for Inflation with Degree-Scale Polarimetry from the South Pole ,NSF| MRI: Development of a 150 GHz Receiver for the BICEP Array CMB Polarimeter ,NSF| Collaborative Research: Imaging the Beginning of Time from the South Pole: Observations with the Full SPUD Array ,NSF| Collaborative Research: BICEP2 and SPUD - A Search for Inflation with Degree-Scale Polarimetry from the South PoleJ. Kang; P. A. R. Ade; Zeeshan Ahmed; Mandana Amiri; Denis Barkats; R. Basu Thakur; Colin A. Bischoff; James J. Bock; H. Boenish; E. Bullock; Victor Buza; J. Cheshire; Jake Connors; J. Cornelison; M. Crumrine; A. Cukierman; E. V. Denison; Marion Dierickx; Lionel Duband; M. Eiben; S. Fatigoni; Jeffrey P. Filippini; S. Fliescher; Neil Goeckner-Wald; D. C. Goldfinger; J. A. Grayson; Paul K. Grimes; G. Hall; Mark Halpern; Sarah M. Harrison; S. Henderson; Sergi R. Hildebrandt; Gene C. Hilton; Johannes Hubmayr; Howard Hui; Kent D. Irwin; Kirit Karkare; E. Karpel; S. Kefeli; S. A. Kernasovskiy; John M Kovac; Chao-Lin Kuo; King Tong Lau; E. M. Leitch; K. G. Megerian; L. Minutolo; Lorenzo Moncelsi; Y. Nakato; Toshiya Namikawa; H. T. Nguyen; Roger O'Brient; R. W. Ogburn; S. Palladino; N. Precup; T. Prouve; C. Pryke; B. Racine; Carl D. Reintsema; S. Richter; Alessandro Schillaci; Benjamin L. Schmitt; R. Schwarz; C. D. Sheehy; Ahmed Soliman; T. St. Germaine; Bryan Steinbach; Rashmikant V. Sudiwala; G. P. Teply; Keith L. Thompson; J. E. Tolan; Carole Tucker; Anthony D. Turner; C. Umiltà; Abigail G. Vieregg; A. Wandui; A. C. Weber; Donald V. Wiebe; J. Willmert; C. L. Wong; W. L. K. Wu; Eui-Hyeok Yang; Ki Won Yoon; Edward D. Young; Che-Hang Yu; Lingzhen Zeng; Chao Zhang; Shengyu Zhang;BICEP3 is a 520 mm aperture on-axis refracting telescope at the South Pole, which observes the polarization of the cosmic microwave background (CMB) at 95 GHz to search for the B-mode signal from inflationary gravitational waves. In addition to this main target, we have developed a low-elevation observation strategy to extend coverage of the Southern sky at the South Pole, where BICEP3 can quickly achieve degree-scale E-mode measurements over a large area. An interesting E-mode measurement is probing a potential polarization anomaly around the CMB Cold Spot. During the austral summer seasons of 2018-19 and 2019-20, BICEP3 observed the sky with a flat mirror to redirect the beams to various low elevation ranges. The preliminary data analysis shows degree-scale E-modes measured with high signal-to-noise ratio. Comment: 12 pages, 10 figures; Figure 7 shows the correct file
Caltech Authors arrow_drop_down Mémoires en Sciences de l'Information et de la Communication; HAL-CEAConference object . 2020https://doi.org/10.48550/arxiv...Article . 2020License: arXiv Non-Exclusive DistributionData sources: Dataciteadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1117/12.2562066&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen 1 citations 1 popularity Average influence Average impulse Average Powered by BIP!more_vert Caltech Authors arrow_drop_down Mémoires en Sciences de l'Information et de la Communication; HAL-CEAConference object . 2020https://doi.org/10.48550/arxiv...Article . 2020License: arXiv Non-Exclusive DistributionData sources: Dataciteadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1117/12.2562066&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book 2015 FrancePublisher:Springer Netherlands Renate Forkel; Alex Guenther; Kirsti Ashworth; Carole Bedos; Claire Delon; J. Lathière; Steffen M. Noe; Elise Potier; Janne Rinne; O. Tchepel; Leiming Zhang;International audience; Volatile organic compounds (VOC) are a relatively minor component of the atmosphere and yet are widely recognized to have important roles in air quality and climate. With the exception of methane, an important greenhouse gas, atmospheric VOC are primarily of interest because of their impact on other atmospheric constituents, including oxidants and aerosol.
https://doi.org/10.1... arrow_drop_down https://doi.org/10.1007/978-94...Part of book or chapter of book . 2015 . Peer-reviewedData sources: CrossrefMémoires en Sciences de l'Information et de la Communication; HAL-CEA; Hal-DiderotPart of book or chapter of book . 2015License: CC BY NCadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/978-94-017-7285-3_8&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu2 citations 2 popularity Average influence Average impulse Average Powered by BIP!more_vert https://doi.org/10.1... arrow_drop_down https://doi.org/10.1007/978-94...Part of book or chapter of book . 2015 . Peer-reviewedData sources: CrossrefMémoires en Sciences de l'Information et de la Communication; HAL-CEA; Hal-DiderotPart of book or chapter of book . 2015License: CC BY NCadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/978-94-017-7285-3_8&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book 2013 FrancePublisher:American Geophysical Union (AGU) Authors: Hirth, Greg; Escartin, Javier; Lin, Jian;Hirth, Greg; Escartin, Javier; Lin, Jian;doi: 10.1029/gm106p0291
An analysis of experimentally determined flow laws for gabbroic rocks indicates that the lower oceanic crust is considerably stronger than commonly assumed in many modeling studies. A combination of experimental, geochemical and petrological constraints suggest that the majority of the lower oceanic crust is almost dry prior to hydrothermal alteration. Several geological and geophysical observations also indicate that the strength of the lower ocean crust approaches that of dry gabbroic rock. These observations are inconsistent with commonly used rheological models for the oceanic lithosphere that incorporate a weak lower crust that decouples a strong upper mantle from a brittle upper crust.
Hal-Diderot arrow_drop_down Mémoires en Sciences de l'Information et de la CommunicationPart of book or chapter of book . 2013https://doi.org/10.1029/gm106p...Part of book or chapter of book . 2013 . Peer-reviewedData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1029/gm106p0291&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu74 citations 74 popularity Top 10% influence Top 10% impulse Top 1% Powered by BIP!more_vert Hal-Diderot arrow_drop_down Mémoires en Sciences de l'Information et de la CommunicationPart of book or chapter of book . 2013https://doi.org/10.1029/gm106p...Part of book or chapter of book . 2013 . Peer-reviewedData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1029/gm106p0291&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book , Other literature type 2020 FrancePublisher:Springer International Publishing Authors: Denis-Didier Rousseau; Christine Hatté;Denis-Didier Rousseau; Christine Hatté;Atmospheric circulation is responsible for the rapid distribution of heat and moisture across the Earth and hence determines our weather and regional climate, today and in the past. During past climate cycles, the atmosphere has been much more dustier, except during the interglacials, inducing uncertainties about the impact of mineral aerosols on the past climate dynamics. There are abundant traces of the combination of past atmospheric dynamics and paleodust cycle such as eolian mineral material transported and deposited in terrestrial archives as loess. Records from loess deposits consistently suggest that atmospheric dynamics was highly variable, during the past climate cycles, much more than presently where the only sources of dust are the major deserts. In this chapter we explained the four main categories of parameters allowing to identify loess deposits as reliable markers for past air circulation. Open image in new window Fig. 13.1 Global distribution of loess sediments and equivalents. 1: loess sediments; 2: loess derivatives (according to Pecsi (1990))
https://academiccomm... arrow_drop_down https://doi.org/10.1007/978-3-...Part of book or chapter of book . 2020 . Peer-reviewedLicense: Springer TDMData sources: CrossrefMémoires en Sciences de l'Information et de la Communication; HAL-CEAPart of book or chapter of book . 2021add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/978-3-030-24982-3_13&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu2 citations 2 popularity Average influence Average impulse Average Powered by BIP!more_vert https://academiccomm... arrow_drop_down https://doi.org/10.1007/978-3-...Part of book or chapter of book . 2020 . Peer-reviewedLicense: Springer TDMData sources: CrossrefMémoires en Sciences de l'Information et de la Communication; HAL-CEAPart of book or chapter of book . 2021add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/978-3-030-24982-3_13&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book 2013 FrancePublisher:Springer Netherlands Authors: Angielczyk, Kenneth, D; Steyer, Jean-Sébastien; Sidor, Christian, A; Smith, Roger; +2 AuthorsAngielczyk, Kenneth, D; Steyer, Jean-Sébastien; Sidor, Christian, A; Smith, Roger; Whatley, Robin, L; Tolan, Stephen;Dicynodont fossils were first collected in the Luangwa Basin, Zambia, in the 1920s, but limited detailed study and taxonomic uncertainty have obscured their biostratigraphic utility and their implications for topics such as dicynodont biogeography and the effects of the end-Permian extinction. Here we present a comprehensive taxonomic revision of the dicynodonts of the Luangwa Basin, taking into account specimens in all major museum collections and new material collected by our team in 2009. We recognize 14 dicynodont species from the Upper Permian Upper Madumabisa Mudstone: Pristerodon mackayi, Endothiodon sp., Diictodon feliceps, Compsodon helmoedi, Emydops sp., Dicynodontoides cf. D. nowacki, a new tusked cistecephalid, cf. Katumbia parringtoni, Kitchinganomodon crassus, Oudenodon bainii, Odontocyclops whaitsi, Dicynodon huenei, Syops vanhoepeni, and a new lystrosaurid. Previous reports of Lystrosaurus in the basin appear to be in error. In addition, we found no significant partitioning of dicynodont taxa in the northern and southern parts of the basin, despite substantial differences in preservation, indicating the presence of a single faunal assemblage in the Upper Permian. The Madumabisa dicynodont assemblage is best correlated with the Cistecephalus Assemblage Zone of South Africa. The shared presence of Dicynodon huenei and possibly Katumbia in the Luangwa Basin and the Ruhuhu Basin of Tanzania suggests that the Tanzanian Usili Formation also can be correlated with the Cistecephalus zone. Interestingly, the Madumabisa assemblage from Zambia is more similar to the coeval assemblage from South Africa, despite its closer geographic proximity to Tanzania. The Karoo and Ruhuhu basins also include more endemic species in the Permian than the Luangwa Basin. The Middle Triassic Ntawere Formation preserves four dicynodont species (Kannemeyeria lophorhinus, “Kannemeyeria” latirostris, Zambiasaurus submersus, Sangusaurus edentatus), which occur at two stratigraphic levels. The lower Ntawere assemblage resembles that of the Omingonde Formation of Namibia in the presence of Kannemeyeria lophorhinus and potentially Dolichuranus (if “K.” latirostris represents this taxon). The upper Ntawere assemblage shares the genus Sangusaurus with that of the Manda beds of Tanzania and includes the endemic Zambiasaurus. Comparisons of these assemblages to the Omingonde and Manda suggest that both are best correlated with the Cynognathus C subzone. When combined with data on other tetrapod taxa, our revised dicynodont assemblages contribute to an emerging picture of broad faunal similarity in southern and eastern Africa during the Late Permian, and increasing differentiation between the South African and other Karoo basins following the end-Permian extinction.
https://doi.org/10.1... arrow_drop_down https://doi.org/10.1007/978-94...Part of book or chapter of book . 2013 . Peer-reviewedLicense: Springer Nature TDMData sources: CrossrefMémoires en Sciences de l'Information et de la Communication; HAL-UPMCPart of book or chapter of book . 2014Full-Text: https://hal.science/hal-02107892/documentMémoires en Sciences de l'Information et de la Communication; Hal-DiderotPart of book or chapter of book . 2014add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/978-94-007-6841-3_7&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu71 citations 71 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!more_vert https://doi.org/10.1... arrow_drop_down https://doi.org/10.1007/978-94...Part of book or chapter of book . 2013 . Peer-reviewedLicense: Springer Nature TDMData sources: CrossrefMémoires en Sciences de l'Information et de la Communication; HAL-UPMCPart of book or chapter of book . 2014Full-Text: https://hal.science/hal-02107892/documentMémoires en Sciences de l'Information et de la Communication; Hal-DiderotPart of book or chapter of book . 2014add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/978-94-007-6841-3_7&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Part of book or chapter of book , Other literature type 2013 FrancePublisher:Springer International Publishing Praeg, D.; Ketzer, J.Marcelo; Augustin, A.H.; Migeon, S.; Ceramicola, S.; Dano, A.; Ducassou, E.; Dupré, S.; Mascle, J.; Rodrigues, L. F.;International audience; On the central Nile deep-sea fan, stratified sediments overlying mass-transport deposits (MTDs) are deformed into slope-parallel seabed undulations associated with fluid seepage. The western part of this system, in water depths of 1,950-2,250 m, is examined using multi-frequency data from hull-mounted and deep-towed swath/profiling systems. Sub-bottom profiles show sub-vertical fluid pipes that terminate both at and below seabed, and gas signatures along fault planes bounding the undulations. Fluid seepage is recorded by high- to intermediate-backscatter patches (HBPs, IBPs) that differ in appearance on multibeam imagery (30 kHz, ≤3 m penetration) and sidescan swaths (170/190 kHz, <0.1 m penetration). Comparison of the two suggests a distinction of (a) buried carbonates (0.1-3 m), (b) broad near-seabed (<0.1 m) carbonate pavements elongate along the undulations, (c) sub-circular areas of seabed seepage up to 300 m across. Four of the latter have narrower gas flares at their edges rising 400-800 m above seabed. These results are consistent with an evolving system of narrow fluid conduits that support the growth and burial of carbonate pavements, shifting over millennial timescales along linear zones parallel to fault planes rooted in MTDs. Sediment deformation above MTDs is inferred to provide pathways for fluid escape, but migration of gas-rich fluids from depth is likely to have facilitated slope destabilisation
https://archimer.ifr... arrow_drop_down ArchiMer - Institutional Archive of IfremerOther literature type . 2014Data sources: ArchiMer - Institutional Archive of Ifremerhttps://doi.org/10.1007/978-3-...Part of book or chapter of book . 2013 . Peer-reviewedLicense: Springer Nature TDMData sources: CrossrefHAL - UPEC / UPEM; HAL-Inserm; Hal-DiderotArticle . 2014add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/978-3-319-00972-8_13&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu11 citations 11 popularity Average influence Average impulse Top 10% Powered by BIP!visibility 7visibility views 7 Powered bymore_vert https://archimer.ifr... arrow_drop_down ArchiMer - Institutional Archive of IfremerOther literature type . 2014Data sources: ArchiMer - Institutional Archive of Ifremerhttps://doi.org/10.1007/978-3-...Part of book or chapter of book . 2013 . Peer-reviewedLicense: Springer Nature TDMData sources: CrossrefHAL - UPEC / UPEM; HAL-Inserm; Hal-DiderotArticle . 2014add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/978-3-319-00972-8_13&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book 2020 FrancePublisher:International Ocean Discovery Program Funded by:ANR | HimalFanANR| HimalFanSebastien Jean Paul Lenard; J. W. Cruz; Christian France-Lanord; Jérôme Lavé; Brendan T Reilly;International audience
https://doi.org/10.1... arrow_drop_down https://doi.org/10.14379/iodp....Part of book or chapter of book . 2020 . Peer-reviewedLicense: CC BYData sources: Crossrefhttps://hal.univ-lorraine.fr/h...Part of book or chapter of bookLicense: CC BYData sources: UnpayWallMémoires en Sciences de l'Information et de la Communication; Hal-DiderotPart of book or chapter of book . 2020add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.14379/iodp.proc.354.203.2020&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routeshybrid 6 citations 6 popularity Top 10% influence Average impulse Top 10% Powered by BIP!more_vert https://doi.org/10.1... arrow_drop_down https://doi.org/10.14379/iodp....Part of book or chapter of book . 2020 . Peer-reviewedLicense: CC BYData sources: Crossrefhttps://hal.univ-lorraine.fr/h...Part of book or chapter of bookLicense: CC BYData sources: UnpayWallMémoires en Sciences de l'Information et de la Communication; Hal-DiderotPart of book or chapter of book . 2020add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.14379/iodp.proc.354.203.2020&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Other literature type , Part of book or chapter of book , Article , Preprint 2013 France, United KingdomPublisher:Springer Netherlands Publicly fundedFunded by:EC | ECLAIRE, EC | PEGASOSEC| ECLAIRE ,EC| PEGASOSChristophe Flechard; Raia Silvia Massad; Benjamin Loubet; Erwan Personne; David Simpson; Jesse O. Bash; Ellen J. Cooter; Eiko Nemitz; Mark A. Sutton;Atmospheric ammonia (NH3) dominates global emissions of total reactive nitrogen (Nr), while emissions from agricultural production systems contribute about two-thirds of global NH3 emissions; the remaining third emanates from oceans, natural vegetation, humans, wild animals and biomass burning. On land, NH3 emitted from the various sources eventually returns to the biosphere by dry deposition to sink areas, predominantly semi-natural vegetation, and by wet and dry deposition as ammonium (NH4+) to all surfaces. However, the land/atmosphere exchange of gaseous NH3 is in fact bi-directional over unfertilized as well as fertilized ecosystems, with periods and areas of emission and deposition alternating in time (diurnal, seasonal) and space (patchwork landscapes). The exchange is controlled by a range of environmental factors, including meteorology, surface layer turbulence, thermodynamics, air and surface heterogeneous-phase chemistry, canopy geometry, plant development stage, leaf age, organic matter decomposition, soil microbial turnover, and, in agricultural systems, by fertilizer application rate, fertilizer type, soil type, crop type, and agricultural management practices. We review the range of processes controlling NH3 emission and uptake in the different parts of the soil-canopy-atmosphere continuum, with NH3 emission potentials defined at the substrate and leaf levels by different [NH4+] / [H+] ratios (Γ). Surface/atmosphere exchange models for NH3 are necessary to compute the temporal and spatial patterns of emissions and deposition at the soil, plant, field, landscape, regional and global scales, in order to assess the multiple environmental impacts of airborne and deposited NH3 and NH4+. Models of soil/vegetation/atmosphere NH3 exchange are reviewed from the substrate and leaf scales to the global scale. They range from simple steady-state, "big leaf" canopy resistance models, to dynamic, multi-layer, multi-process, multi-chemical species schemes. Their level of complexity depends on their purpose, the spatial scale at which they are applied, the current level of parameterization, and the availability of the input data they require. State-of-the-art solutions for determining the emission/sink Γ potentials through the soil/canopy system include coupled, interactive chemical transport models (CTM) and soil/ecosystem modelling at the regional scale. However, it remains a matter for debate to what extent realistic options for future regional and global models should be based on process-based mechanistic versus empirical and regression-type models. Further discussion is needed on the extent and timescale by which new approaches can be used, such as integration with ecosystem models and satellite observations.
Biogeosciences; NERC... arrow_drop_down Biogeosciences; NERC Open Research ArchiveArticle . 2013 . Peer-reviewedhttps://doi.org/10.1007/978-94...Part of book or chapter of book . 2013 . Peer-reviewedLicense: CC BY NCMémoires en Sciences de l'Information et de la CommunicationArticle . 2013Full-Text: https://hal.science/hal-01190540/documentHAL - UPEC / UPEM; HAL-Pasteur; HAL-Inserm; Hal-DiderotArticle . 2013Mémoires en Sciences de l'Information et de la CommunicationPart of book or chapter of book . 2015HAL - UPEC / UPEM; HAL-Pasteur; HAL-Inserm; Hal-DiderotPart of book or chapter of book . 2015add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/978-94-017-7285-3_2&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routesgold 108 citations 108 popularity Top 10% influence Top 10% impulse Top 1% Powered by BIP!visibility 3visibility views 3 download downloads 35 Powered bymore_vert Biogeosciences; NERC... arrow_drop_down Biogeosciences; NERC Open Research ArchiveArticle . 2013 . Peer-reviewedhttps://doi.org/10.1007/978-94...Part of book or chapter of book . 2013 . Peer-reviewedLicense: CC BY NCMémoires en Sciences de l'Information et de la CommunicationArticle . 2013Full-Text: https://hal.science/hal-01190540/documentHAL - UPEC / UPEM; HAL-Pasteur; HAL-Inserm; Hal-DiderotArticle . 2013Mémoires en Sciences de l'Information et de la CommunicationPart of book or chapter of book . 2015HAL - UPEC / UPEM; HAL-Pasteur; HAL-Inserm; Hal-DiderotPart of book or chapter of book . 2015add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/978-94-017-7285-3_2&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu