Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7485
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dc.contributor.authorallRaffaele, R.; Università di Catania, Italyen
dc.contributor.authorallSapin, M.; Institut de Physique du Globe de Paris, Franceen
dc.contributor.authorallLaigle, M.; Institut de Physique du Globe de Paris, Franceen
dc.contributor.authorallScarfì, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
dc.contributor.authorallCharvis, P.; Université Nice Sophia Antipolis, Franceen
dc.contributor.authorallDiaz, J.; Universitat de Barcelona, Spainen
dc.contributor.authorallImposa, S.; Università di Catania, Italyen
dc.contributor.editorallEAGE - European association of geoscientists & engineersen
dc.date.accessioned2012-01-23T14:43:39Zen
dc.date.available2012-01-23T14:43:39Zen
dc.date.issued2012-04-03en
dc.identifier.urihttp://hdl.handle.net/2122/7485en
dc.description.abstractIn this study, we present results of the investigation programme SISMANTILLES I, conducted from November 1999 to January 2002, on the Lesser Antilles Arc. We analyzed seismicity by using the data recorded by a combined on- and offshore network that integrated the local volcano-seismological observatories of the Institut de Physique du Globe de Paris (IPGP). The SISMANTILLES I landward network comprised 43 three-component temporary stations. To improve azimuth coverage in earthquake location, it was complemented by 31 OBS. A data-set of 155 well located earthquakes has been used to study the relationship between tectonic structures and seismicity. In particular, to obtain precise hypocenter locations, we applied the concept of minimum 1D model which incorporates the iterative simultaneous inversion of velocity and hypocenter parameters. To partly estimate the huge structural heterogeneity of the Lesser Antilles Subduction Zone, the minimum 1D model is complemented by station corrections which take into account near surface velocity heterogeneity. The relocated hypocenters improve our knowledge on the subduction zone since they have smaller uncertainties with respect to the permanent array locations. The vertical depth sections, perpendicular to the arc, will help define the slab structure and the dip angle.en
dc.language.isoEnglishen
dc.relation.ispartofGeosciences: Making the most of the Earth’s resourcesen
dc.subjectSeismic Interpretationen
dc.subjectSeismic Data Acquisition and Processingen
dc.subjectNear-Surface structureen
dc.titleAccurate Hypocenter Determination in Lesser Antilles Region from the Sismantilles I Experimenen
dc.typeExtended abstracten
dc.description.statusSubmitteden
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.02. Geodynamicsen
dc.description.ConferenceLocationSaint Petersburg, Russiaen
dc.relation.referencesDeMets, C., Jansma P. E., Mattioli G. S., Dixon T. H., Farina F., Bilham R., Calais E. and Mann P. [2000] GPS geodetic constraints on Caribbean-North America plate motion. Geophysical Research Letters, 27, 437-440. Bengoubou-Valerius, M., Bazin, S., Bertil, D., Beauducel, F. and Bosson A. [2008] CDSA: a new seismological data center for the French Lesser Antilles. Seismological Research Letters, 79, 90-102. Dorel, J. [1981] Seismicity and seismic gaps in the Lesser Antilles arc and earthquake hazards in Guadeloupe. Geophysical Journal of the Royal Astronomical Society, 67, 679-696. Kissling, E., Ellworth W.L., Eberhart-Phillips D. and Kradolfer U., [1994] Initial reference models in local earthquake tomography. Journal of Geophysical Research, 99, 19,635−19,646. Laigle, M., Becel, A., Kopp, H., Lebrun, J-F, and Klaeschen, D. [2010] Along-arc segmentation and interaction of subducting ridges with the Lesser Antilles Subduction forearc crust revealed by MCS imaging. EGU General Assembly, Vienna, Austria.en
dc.description.obiettivoSpecifico3.2. Tettonica attivaen
dc.description.fulltextopenen
dc.contributor.authorRaffaele, R.en
dc.contributor.authorSapin, M.en
dc.contributor.authorLaigle, M.en
dc.contributor.authorScarfì, L.en
dc.contributor.authorCharvis, P.en
dc.contributor.authorDiaz, J.en
dc.contributor.authorImposa, S.en
dc.contributor.departmentUniversità di Catania, Italyen
dc.contributor.departmentInstitut de Physique du Globe de Paris, Franceen
dc.contributor.departmentInstitut de Physique du Globe de Paris, Franceen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
dc.contributor.departmentUniversité Nice Sophia Antipolis, Franceen
dc.contributor.departmentUniversitat de Barcelona, Spainen
dc.contributor.departmentUniversità di Catania, Italyen
item.openairetypeExtended abstract-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptDipartimento di Scienze Geologiche, Università di Catania, Italy-
crisitem.author.deptInstitut de Physique du Globe de Paris, France-
crisitem.author.deptInstitut de Physique du Globe de Paris, France-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.deptUniversité Nice Sophia Antipolis, France-
crisitem.author.deptInstitut de Ciències de La Terra Jaume Almera, Spain-
crisitem.author.deptDipartimento di Scienze Geologiche, Università di Catania, Italy-
crisitem.author.orcid0000-0002-5995-3880-
crisitem.author.orcid0000-0003-1738-1850-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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