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description Publicationkeyboard_double_arrow_right Part of book or chapter of book 2013 SwitzerlandPublisher:Cambridge University Press (CUP) Authors: Bonadonna, Costanza; Costa, Antonio;Bonadonna, Costanza; Costa, Antonio;Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1017/cbo978...Part of book or chapter of book . 2013 . Peer-reviewedLicense: Cambridge Core User AgreementData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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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=10.1017/cbo9781139021562.009&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu24 citations 24 popularity Top 10% influence Average impulse Top 10% Powered by BIP!more_vert Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1017/cbo978...Part of book or chapter of book . 2013 . Peer-reviewedLicense: Cambridge Core User AgreementData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book 2014 France EnglishPublisher:HAL CCSD Authors: Banos, Arnaud; Beck, Elise; Glatron, Sandrine; Mudu, Pierpaolo;Banos, Arnaud; Beck, Elise; Glatron, Sandrine; Mudu, Pierpaolo;International audience; Industrial development can generate hazardous situations – in particular, when there is a need to deal with dangerous substances, such as those in chemical or petrochemical plants. Too often, these industries are located in the heart of urbanized areas with high-density populations, as urbanization intrudes on the hazardous sites (originally established outside of cities). Protecting civil populations from these risks – either through precautionary measures or special crisis management plans, if a catastrophe occurs – is a key issue. To better protect citizens, identifying the risks to which they are exposed and also how they perceive the risks in their area can help authorities and stakeholders better understand the risks (Glatron & Beck, 2008). Adequate knowledge of these risks can also dissuade populations from settling in certain zones and thus lower their vulnerability. Finally, authorities need to assess the exposure of populations to hazards – through modelling – to set up appropriate and efficient risk management plans based on land planning. The present chapter – founded on responses to a questionnaire-based investigation (see the Annex) carried out in the Milazzo–Valle del Mela area of Sicily, in 2008 – explores two main aspects of exposure assessment: space-time-pattern methodological challenges and results of individual space-time activity data extracted from the investigation in the Milazzo–Valle del Mela area.
Mémoires en Sciences... arrow_drop_down Mémoires en Sciences de l'Information et de la CommunicationPart of book or chapter of book . 2014License: CC BY NC NDFull-Text: https://hal.science/hal-01102091/documentHyper Article en Ligne - Sciences de l'Homme et de la Société; Hal-DiderotPart of book or chapter of book . 2014License: CC BY NC NDAll 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=od______2592::d4343022bf454bbdad24b40dbcf1191c&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu0 citations 0 popularity Average influence Average impulse Average Powered by BIP!more_vert Mémoires en Sciences... arrow_drop_down Mémoires en Sciences de l'Information et de la CommunicationPart of book or chapter of book . 2014License: CC BY NC NDFull-Text: https://hal.science/hal-01102091/documentHyper Article en Ligne - Sciences de l'Homme et de la Société; Hal-DiderotPart of book or chapter of book . 2014License: CC BY NC NDAll 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=od______2592::d4343022bf454bbdad24b40dbcf1191c&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book 2004 SwitzerlandPublisher:Elsevier BV Authors: Kindler, Pascal; Hearty, Paul J.;Kindler, Pascal; Hearty, Paul J.;This chapter focuses on the three-dimensional mosaic making up the islands. The chapter uses the stratigraphic scheme, which differs from the formal lithostratigraphic column. It has become clear that there is variability among Bahamian islands with respect to their stratigraphic architecture, and that there are patterns to this variability. Such observations present in the chapter provide tentative classification of islands where one can find or expect to find different types of stratigraphic architecture. Although the classification is still a hypothesis, which one can test by studying more Bahamian islands, the chapter includes it as an organizer and provides a potential framework for (1) understanding Bahamian islands fully, and (2) comparing Bahamian islands to other kinds of carbonate islands. The architecture of Bahamian islands shows that they grow by lateral accretion or vertical stacking depending on their exposure to the open ocean and the width of the outer platform.
Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1016/s0070-...Part of book or chapter of book . 2004 . Peer-reviewedLicense: Elsevier 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.
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For further information contact us at helpdesk@openaire.eu32 citations 32 popularity Average influence Top 10% impulse Top 10% Powered by BIP!more_vert Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1016/s0070-...Part of book or chapter of book . 2004 . Peer-reviewedLicense: Elsevier 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.
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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=10.1016/s0070-4571(04)80024-4&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 SwitzerlandPublisher:Springer International Publishing Authors: Engielle Mae Paguican; Matteo Roverato; Hidetsugu Yoshida;Engielle Mae Paguican; Matteo Roverato; Hidetsugu Yoshida;Field observations of volcanic debris avalanche (VDA) morphology, sedimentology, and structural features have inspired several hypotheses on their dynamic behaviour. These include plug flow, translational slide, and sliding along multiple shear zones, none of which involve large-scale turbulence during transport. The plug flow model shows normal gradation in the plug, and reverse grading in the laminar boundary layers. During translational sliding, spreading of the mass is accommodated by listric normal faults that flatten into a main sliding plane at the base of or within the avalanche body. Multiple shear zones include progressive fragmentation within the avalanching mass, resulting in pockets of shear and slip. We present case studies for each model and hypotheses for the formation of flowbands on the deposit surface. Processes involved during emplacement include disintegration, dynamic fragmentation, and matrix injection. Near the base, bulldozing and incorporation of substrata change the composition and behaviour of the VDA. In extreme cases, VDAs transform into lahars if sufficient water is available for entrainment. Post-emplacement, lahars can also happen, e.g., through debris dewatering, loading of saturated substrata or in the case of landslide dam failure. VDA also create secondary slides when deflected by topographic barriers or when the margins are oversteepened.
Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1007/978-3-...Part of book or chapter of book . 2020 . Peer-reviewedLicense: Springer Nature 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.
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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=10.1007/978-3-030-57411-6_7&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu6 citations 6 popularity Top 10% influence Average impulse Top 10% Powered by BIP!more_vert Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1007/978-3-...Part of book or chapter of book . 2020 . Peer-reviewedLicense: Springer Nature 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=10.1007/978-3-030-57411-6_7&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 2012 SwitzerlandPublisher:Wiley Authors: Ruchonnet, Cyril; Kindler, Pascal;Ruchonnet, Cyril; Kindler, Pascal;Detailed sequence and facies analyses of eleven stratigraphic sections, positioned on two platform to basin transects, on the Ragusa ramp (Sicily, Italy) demonstrates that two facies models must be used to describe the internal architecture of this carbonate edifice near the Serravallian/Tortonian boundary. Seven facies zones, based on the paleobathymetric position of the carbonate-producing biota, have been defined and described for each of these stages. During the late Serravallian, the inner ramp was characterized mainly by small epiphytic biota of the foramol association, whereas the middle ramp was dominated by rhodoliths and minor benthic foraminifera, bryozoans, barnacles, serpulids and echinoids. In contrast, during the early Tortonian, the inner ramp was characterized by a chlorozoan biota (Porites, Halimeda), and the middle ramp by branching Corallinacea and rhodoliths. This seemingly minor modification in the type and locus of carbonate production, and the associated changes in hydrodynamism, had profound consequences on the overall geometry of the platform which evolved from a distally steepened ramp, in the late Serravallian, to a geometry approaching that of flat-topped platform in the early Tortonian.
Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1002/978111...Other literature type . 2012License: Wiley 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.
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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=10.1002/9781118398364.ch5&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu6 citations 6 popularity Average influence Average impulse Average Powered by BIP!more_vert Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1002/978111...Other literature type . 2012License: Wiley 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.
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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=10.1002/9781118398364.ch5&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book 1994 SwitzerlandPublisher:Springer Netherlands Authors: Davaud, Eric Jean; Strasser, Andréas; Jedoui, Younes;Davaud, Eric Jean; Strasser, Andréas; Jedoui, Younes;The Sebkha el Melah, located near the Libyan-Tunisian border, is fringed by a relict stromatolite-serpulid belt. These bioherms developed 5500 years ago during the Flandrian sea-level highstand when the area of the present-day sebkha was covered by a wide restricted lagoon. Relict lagoonal beaches and spits, mainly composed of cerebroid ooids and cerithid gastropods, are flanked by mushroom-shaped stromatolites reaching up to 50 cm in height. These stromatolites grew on top of small serpulid bioherms as well as on top of beachrock and beachrock blocks in a shallow subtidal pre-evaporitic realm. The primary porosity of these bioherms is obliterated by botryoidal and spherulitic aragonite, probably of microbial origin. This sub-Recent association of stromatolites, serpulid bioherms and cerebroid ooids provides a useful additional model for the interpretation of upper Paleozoic deposits, where similar facies have been described.
Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1007/978-94...Part of book or chapter of book . 1994 . 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.
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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=10.1007/978-94-011-1124-9_6&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu20 citations 20 popularity Top 10% influence Average impulse Average Powered by BIP!more_vert Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1007/978-94...Part of book or chapter of book . 1994 . 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.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book 2020 SwitzerlandPublisher:Springer International Publishing Authors: Moscariello, Andrea;Moscariello, Andrea;The landscape of the Geneva Basin, located in the south-westernmost part of the Swiss Plateau between the northern end of the Prealps and the Jura, results from the long-term, continuous tectonic deformation of the Alpine foreland and surface processes reflecting alternation of glacial and interglacial periods. The main geomorphological elements of the Geneva Basin can be thus divided in: (i) tectonically controlled features, associated with the north-westernmost compressive Alpine tectonics represented by SW-NE oriented ridges interrupted by NW-SE lineaments; (ii) glacially related erosional and depositional features; and (iii) postglacial establishment of the present day hydrographic network. Responsible land-use planning over the last centuries resulted in a region internationally known for a balance between urban and industry expansion, agricultural activities and nature preservation areas, which is ensuring both economic and landscape attractiveness of the Geneva Basin.
Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1007/978-3-...Part of book or chapter of book . 2020 . 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.
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For further information contact us at helpdesk@openaire.eu3 citations 3 popularity Average influence Average impulse Average Powered by BIP!more_vert Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1007/978-3-...Part of book or chapter of book . 2020 . 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.
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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=10.1007/978-3-030-43203-4_6&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 Italy, SwitzerlandPublisher:Cambridge University Press (CUP) Jenkins S. F.; Wilson T.; Magill C.; Miller V.; Stewart C.; Blong R.; Marzocchi W.; Boulton M.; Bonadonna C.; Costa A.;handle: 11588/815807
http://www.preventio... arrow_drop_down https://doi.org/10.1017/cbo978...Part of book or chapter of book . 2015 . Peer-reviewedLicense: Cambridge Core User AgreementData sources: CrossrefArchivio della ricerca - Università degli studi di Napoli Federico IIPart of book or chapter of book . 2015Archivio della ricerca - Università degli studi di Napoli Federico IIPart 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=10.1017/cbo9781316276273.005&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu61 citations 61 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!more_vert http://www.preventio... arrow_drop_down https://doi.org/10.1017/cbo978...Part of book or chapter of book . 2015 . Peer-reviewedLicense: Cambridge Core User AgreementData sources: CrossrefArchivio della ricerca - Università degli studi di Napoli Federico IIPart of book or chapter of book . 2015Archivio della ricerca - Università degli studi di Napoli Federico IIPart 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=10.1017/cbo9781316276273.005&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book 1990 SwitzerlandPublisher:Springer Berlin Heidelberg Authors: Wolf, Frank; Fontboté, Lluís; Amstutz, G.C.;Wolf, Frank; Fontboté, Lluís; Amstutz, G.C.;The Susana copper deposit is located at an elevation of 860 m above sea level in the coastal Cordillera of northern Chile (Carolina de Michilla district), 110 km north of Antofagasta at 70°10′W and 22°40′S. Initial mining began in 1981 by surface mining methods with production coming from one open bit. Due to subsequent geologic reconnaissance that resulted in the discovery of a mineralized breccia pipe structure, underground mining started in 1983. By 1983, 36000 m of drilling had shown the presence of 8 million metric tons of oxide/sulfide ore averaging 2% copper at 0.5% cutoff (Valdebenito 1983) with probable reserves several million tonnes greater. Mine production in 1985 was 1700 mt/day with Cu >3% and 20 g/mt Ag.
Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1007/978-3-...Part of book or chapter of book . 1990 . 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.
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For further information contact us at helpdesk@openaire.eu11 citations 11 popularity Average influence Average impulse Average Powered by BIP!more_vert Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1007/978-3-...Part of book or chapter of book . 1990 . 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.
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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=10.1007/978-3-642-88282-1_24&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book 2012 SwitzerlandPublisher:Society of Economic Geologists Authors: Kouzmanov, Kalin; Pokrovski, Gleb S.;Kouzmanov, Kalin; Pokrovski, Gleb S.;doi: 10.5382/sp.16.22
Extensive research during the 20th century on porphyry Cu (-Mo-Au) deposits has revealed the following major geodynamic, petrological, mineralogical, and geochemical features that characterize these deposits: (1) these systems commonly occur in continental and oceanic magmatic arcs or in collisional orogenic belts; (2) they have spatial and genetic relationships to basaltic-to-felsic magmas emplaced in the upper 10 km of the crust; (3) lateral and vertical alteration-mineralization zoning consists of a Cu (± Mo ± Au) ore shell in the shallow portion of a potassic alteration zone, produced by magmatic fluids; this can be overprinted by phyllic alteration, also largely magmatic in signature, that in turn may be overprinted by argillic alteration, with a dominantly meteoric signature; (4) associated deposits such as skarns, Cordilleran vein, and high and intermediate sulfidation epithermal deposits may occur above or adjacent to porphyry orebodies; (5) porphyry systems form from S- and metal-rich, single-phase aqueous fluid of moderate salinity (2–10 wt % NaCl equiv) exsolved from magmas; during its ascent toward the surface this fluid undergoes a variety of processes that can cause metal precipitation, including decompression, phase separation, cooling, interaction with host rocks, and mixing. In the last 20 years, novel microanalytical techniques for in situ characterization of individual fluid inclusions have provided direct evidence for the chemical and phase composition plus metal content of ore-forming fluids in porphyry systems. In this contribution, we compile a large dataset of published fluid inclusion compositions from more than 30 deposits of the porphyry-skarn-epithermal suite.
Archive ouverte UNIG... arrow_drop_down https://doi.org/10.5382/sp.16....Part of book or chapter of book . 2012 . 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.
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For further information contact us at helpdesk@openaire.eu99 citations 99 popularity Top 1% influence Top 10% impulse Top 10% Powered by BIP!more_vert Archive ouverte UNIG... arrow_drop_down https://doi.org/10.5382/sp.16....Part of book or chapter of book . 2012 . 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.
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description Publicationkeyboard_double_arrow_right Part of book or chapter of book 2013 SwitzerlandPublisher:Cambridge University Press (CUP) Authors: Bonadonna, Costanza; Costa, Antonio;Bonadonna, Costanza; Costa, Antonio;Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1017/cbo978...Part of book or chapter of book . 2013 . Peer-reviewedLicense: Cambridge Core User AgreementData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eu24 citations 24 popularity Top 10% influence Average impulse Top 10% Powered by BIP!more_vert Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1017/cbo978...Part of book or chapter of book . 2013 . Peer-reviewedLicense: Cambridge Core User AgreementData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book 2014 France EnglishPublisher:HAL CCSD Authors: Banos, Arnaud; Beck, Elise; Glatron, Sandrine; Mudu, Pierpaolo;Banos, Arnaud; Beck, Elise; Glatron, Sandrine; Mudu, Pierpaolo;International audience; Industrial development can generate hazardous situations – in particular, when there is a need to deal with dangerous substances, such as those in chemical or petrochemical plants. Too often, these industries are located in the heart of urbanized areas with high-density populations, as urbanization intrudes on the hazardous sites (originally established outside of cities). Protecting civil populations from these risks – either through precautionary measures or special crisis management plans, if a catastrophe occurs – is a key issue. To better protect citizens, identifying the risks to which they are exposed and also how they perceive the risks in their area can help authorities and stakeholders better understand the risks (Glatron & Beck, 2008). Adequate knowledge of these risks can also dissuade populations from settling in certain zones and thus lower their vulnerability. Finally, authorities need to assess the exposure of populations to hazards – through modelling – to set up appropriate and efficient risk management plans based on land planning. The present chapter – founded on responses to a questionnaire-based investigation (see the Annex) carried out in the Milazzo–Valle del Mela area of Sicily, in 2008 – explores two main aspects of exposure assessment: space-time-pattern methodological challenges and results of individual space-time activity data extracted from the investigation in the Milazzo–Valle del Mela area.
Mémoires en Sciences... arrow_drop_down Mémoires en Sciences de l'Information et de la CommunicationPart of book or chapter of book . 2014License: CC BY NC NDFull-Text: https://hal.science/hal-01102091/documentHyper Article en Ligne - Sciences de l'Homme et de la Société; Hal-DiderotPart of book or chapter of book . 2014License: CC BY NC NDAll 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=od______2592::d4343022bf454bbdad24b40dbcf1191c&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu0 citations 0 popularity Average influence Average impulse Average Powered by BIP!more_vert Mémoires en Sciences... arrow_drop_down Mémoires en Sciences de l'Information et de la CommunicationPart of book or chapter of book . 2014License: CC BY NC NDFull-Text: https://hal.science/hal-01102091/documentHyper Article en Ligne - Sciences de l'Homme et de la Société; Hal-DiderotPart of book or chapter of book . 2014License: CC BY NC NDAll 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=od______2592::d4343022bf454bbdad24b40dbcf1191c&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book 2004 SwitzerlandPublisher:Elsevier BV Authors: Kindler, Pascal; Hearty, Paul J.;Kindler, Pascal; Hearty, Paul J.;This chapter focuses on the three-dimensional mosaic making up the islands. The chapter uses the stratigraphic scheme, which differs from the formal lithostratigraphic column. It has become clear that there is variability among Bahamian islands with respect to their stratigraphic architecture, and that there are patterns to this variability. Such observations present in the chapter provide tentative classification of islands where one can find or expect to find different types of stratigraphic architecture. Although the classification is still a hypothesis, which one can test by studying more Bahamian islands, the chapter includes it as an organizer and provides a potential framework for (1) understanding Bahamian islands fully, and (2) comparing Bahamian islands to other kinds of carbonate islands. The architecture of Bahamian islands shows that they grow by lateral accretion or vertical stacking depending on their exposure to the open ocean and the width of the outer platform.
Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1016/s0070-...Part of book or chapter of book . 2004 . Peer-reviewedLicense: Elsevier 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.
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For further information contact us at helpdesk@openaire.eu32 citations 32 popularity Average influence Top 10% impulse Top 10% Powered by BIP!more_vert Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1016/s0070-...Part of book or chapter of book . 2004 . Peer-reviewedLicense: Elsevier 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.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book 2020 SwitzerlandPublisher:Springer International Publishing Authors: Engielle Mae Paguican; Matteo Roverato; Hidetsugu Yoshida;Engielle Mae Paguican; Matteo Roverato; Hidetsugu Yoshida;Field observations of volcanic debris avalanche (VDA) morphology, sedimentology, and structural features have inspired several hypotheses on their dynamic behaviour. These include plug flow, translational slide, and sliding along multiple shear zones, none of which involve large-scale turbulence during transport. The plug flow model shows normal gradation in the plug, and reverse grading in the laminar boundary layers. During translational sliding, spreading of the mass is accommodated by listric normal faults that flatten into a main sliding plane at the base of or within the avalanche body. Multiple shear zones include progressive fragmentation within the avalanching mass, resulting in pockets of shear and slip. We present case studies for each model and hypotheses for the formation of flowbands on the deposit surface. Processes involved during emplacement include disintegration, dynamic fragmentation, and matrix injection. Near the base, bulldozing and incorporation of substrata change the composition and behaviour of the VDA. In extreme cases, VDAs transform into lahars if sufficient water is available for entrainment. Post-emplacement, lahars can also happen, e.g., through debris dewatering, loading of saturated substrata or in the case of landslide dam failure. VDA also create secondary slides when deflected by topographic barriers or when the margins are oversteepened.
Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1007/978-3-...Part of book or chapter of book . 2020 . Peer-reviewedLicense: Springer Nature 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.
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For further information contact us at helpdesk@openaire.eu6 citations 6 popularity Top 10% influence Average impulse Top 10% Powered by BIP!more_vert Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1007/978-3-...Part of book or chapter of book . 2020 . Peer-reviewedLicense: Springer Nature 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.
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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=10.1007/978-3-030-57411-6_7&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 2012 SwitzerlandPublisher:Wiley Authors: Ruchonnet, Cyril; Kindler, Pascal;Ruchonnet, Cyril; Kindler, Pascal;Detailed sequence and facies analyses of eleven stratigraphic sections, positioned on two platform to basin transects, on the Ragusa ramp (Sicily, Italy) demonstrates that two facies models must be used to describe the internal architecture of this carbonate edifice near the Serravallian/Tortonian boundary. Seven facies zones, based on the paleobathymetric position of the carbonate-producing biota, have been defined and described for each of these stages. During the late Serravallian, the inner ramp was characterized mainly by small epiphytic biota of the foramol association, whereas the middle ramp was dominated by rhodoliths and minor benthic foraminifera, bryozoans, barnacles, serpulids and echinoids. In contrast, during the early Tortonian, the inner ramp was characterized by a chlorozoan biota (Porites, Halimeda), and the middle ramp by branching Corallinacea and rhodoliths. This seemingly minor modification in the type and locus of carbonate production, and the associated changes in hydrodynamism, had profound consequences on the overall geometry of the platform which evolved from a distally steepened ramp, in the late Serravallian, to a geometry approaching that of flat-topped platform in the early Tortonian.
Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1002/978111...Other literature type . 2012License: Wiley 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.
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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=10.1002/9781118398364.ch5&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu6 citations 6 popularity Average influence Average impulse Average Powered by BIP!more_vert Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1002/978111...Other literature type . 2012License: Wiley 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.
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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=10.1002/9781118398364.ch5&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book 1994 SwitzerlandPublisher:Springer Netherlands Authors: Davaud, Eric Jean; Strasser, Andréas; Jedoui, Younes;Davaud, Eric Jean; Strasser, Andréas; Jedoui, Younes;The Sebkha el Melah, located near the Libyan-Tunisian border, is fringed by a relict stromatolite-serpulid belt. These bioherms developed 5500 years ago during the Flandrian sea-level highstand when the area of the present-day sebkha was covered by a wide restricted lagoon. Relict lagoonal beaches and spits, mainly composed of cerebroid ooids and cerithid gastropods, are flanked by mushroom-shaped stromatolites reaching up to 50 cm in height. These stromatolites grew on top of small serpulid bioherms as well as on top of beachrock and beachrock blocks in a shallow subtidal pre-evaporitic realm. The primary porosity of these bioherms is obliterated by botryoidal and spherulitic aragonite, probably of microbial origin. This sub-Recent association of stromatolites, serpulid bioherms and cerebroid ooids provides a useful additional model for the interpretation of upper Paleozoic deposits, where similar facies have been described.
Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1007/978-94...Part of book or chapter of book . 1994 . 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.
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For further information contact us at helpdesk@openaire.eu20 citations 20 popularity Top 10% influence Average impulse Average Powered by BIP!more_vert Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1007/978-94...Part of book or chapter of book . 1994 . 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.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book 2020 SwitzerlandPublisher:Springer International Publishing Authors: Moscariello, Andrea;Moscariello, Andrea;The landscape of the Geneva Basin, located in the south-westernmost part of the Swiss Plateau between the northern end of the Prealps and the Jura, results from the long-term, continuous tectonic deformation of the Alpine foreland and surface processes reflecting alternation of glacial and interglacial periods. The main geomorphological elements of the Geneva Basin can be thus divided in: (i) tectonically controlled features, associated with the north-westernmost compressive Alpine tectonics represented by SW-NE oriented ridges interrupted by NW-SE lineaments; (ii) glacially related erosional and depositional features; and (iii) postglacial establishment of the present day hydrographic network. Responsible land-use planning over the last centuries resulted in a region internationally known for a balance between urban and industry expansion, agricultural activities and nature preservation areas, which is ensuring both economic and landscape attractiveness of the Geneva Basin.
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For further information contact us at helpdesk@openaire.eu3 citations 3 popularity Average influence Average impulse Average Powered by BIP!more_vert Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1007/978-3-...Part of book or chapter of book . 2020 . 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.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book 2015 Italy, SwitzerlandPublisher:Cambridge University Press (CUP) Jenkins S. F.; Wilson T.; Magill C.; Miller V.; Stewart C.; Blong R.; Marzocchi W.; Boulton M.; Bonadonna C.; Costa A.;handle: 11588/815807
http://www.preventio... arrow_drop_down https://doi.org/10.1017/cbo978...Part of book or chapter of book . 2015 . Peer-reviewedLicense: Cambridge Core User AgreementData sources: CrossrefArchivio della ricerca - Università degli studi di Napoli Federico IIPart of book or chapter of book . 2015Archivio della ricerca - Università degli studi di Napoli Federico IIPart 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.
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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=10.1017/cbo9781316276273.005&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu61 citations 61 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!more_vert http://www.preventio... arrow_drop_down https://doi.org/10.1017/cbo978...Part of book or chapter of book . 2015 . Peer-reviewedLicense: Cambridge Core User AgreementData sources: CrossrefArchivio della ricerca - Università degli studi di Napoli Federico IIPart of book or chapter of book . 2015Archivio della ricerca - Università degli studi di Napoli Federico IIPart 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=10.1017/cbo9781316276273.005&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book 1990 SwitzerlandPublisher:Springer Berlin Heidelberg Authors: Wolf, Frank; Fontboté, Lluís; Amstutz, G.C.;Wolf, Frank; Fontboté, Lluís; Amstutz, G.C.;The Susana copper deposit is located at an elevation of 860 m above sea level in the coastal Cordillera of northern Chile (Carolina de Michilla district), 110 km north of Antofagasta at 70°10′W and 22°40′S. Initial mining began in 1981 by surface mining methods with production coming from one open bit. Due to subsequent geologic reconnaissance that resulted in the discovery of a mineralized breccia pipe structure, underground mining started in 1983. By 1983, 36000 m of drilling had shown the presence of 8 million metric tons of oxide/sulfide ore averaging 2% copper at 0.5% cutoff (Valdebenito 1983) with probable reserves several million tonnes greater. Mine production in 1985 was 1700 mt/day with Cu >3% and 20 g/mt Ag.
Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1007/978-3-...Part of book or chapter of book . 1990 . 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.
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For further information contact us at helpdesk@openaire.eu11 citations 11 popularity Average influence Average impulse Average Powered by BIP!more_vert Archive ouverte UNIG... arrow_drop_down https://doi.org/10.1007/978-3-...Part of book or chapter of book . 1990 . 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.
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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=10.1007/978-3-642-88282-1_24&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book 2012 SwitzerlandPublisher:Society of Economic Geologists Authors: Kouzmanov, Kalin; Pokrovski, Gleb S.;Kouzmanov, Kalin; Pokrovski, Gleb S.;doi: 10.5382/sp.16.22
Extensive research during the 20th century on porphyry Cu (-Mo-Au) deposits has revealed the following major geodynamic, petrological, mineralogical, and geochemical features that characterize these deposits: (1) these systems commonly occur in continental and oceanic magmatic arcs or in collisional orogenic belts; (2) they have spatial and genetic relationships to basaltic-to-felsic magmas emplaced in the upper 10 km of the crust; (3) lateral and vertical alteration-mineralization zoning consists of a Cu (± Mo ± Au) ore shell in the shallow portion of a potassic alteration zone, produced by magmatic fluids; this can be overprinted by phyllic alteration, also largely magmatic in signature, that in turn may be overprinted by argillic alteration, with a dominantly meteoric signature; (4) associated deposits such as skarns, Cordilleran vein, and high and intermediate sulfidation epithermal deposits may occur above or adjacent to porphyry orebodies; (5) porphyry systems form from S- and metal-rich, single-phase aqueous fluid of moderate salinity (2–10 wt % NaCl equiv) exsolved from magmas; during its ascent toward the surface this fluid undergoes a variety of processes that can cause metal precipitation, including decompression, phase separation, cooling, interaction with host rocks, and mixing. In the last 20 years, novel microanalytical techniques for in situ characterization of individual fluid inclusions have provided direct evidence for the chemical and phase composition plus metal content of ore-forming fluids in porphyry systems. In this contribution, we compile a large dataset of published fluid inclusion compositions from more than 30 deposits of the porphyry-skarn-epithermal suite.
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For further information contact us at helpdesk@openaire.eu99 citations 99 popularity Top 1% influence Top 10% impulse Top 10% Powered by BIP!more_vert Archive ouverte UNIG... arrow_drop_down https://doi.org/10.5382/sp.16....Part of book or chapter of book . 2012 . 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.
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