Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8323
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dc.contributor.authorallMaesano, F. E.en
dc.contributor.authorallToscani, G.; Dipartimento di Scienze della Terra e dell'Ambiente, Università di Paviaen
dc.contributor.authorallBurrato, P.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallMirabella, F.; Dipartimento di Scienze della Terra, Università di Perugiaen
dc.contributor.authorallD'ambrogi, C.; ISPRA - Servizio Geologico d'Italiaen
dc.contributor.authorallBasili, R.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.date.accessioned2012-10-22T06:15:32Zen
dc.date.available2012-10-22T06:15:32Zen
dc.date.issued2013en
dc.identifier.urihttp://hdl.handle.net/2122/8323en
dc.description.abstractWe present a reconstruction of the central Marche thrust system in the central-northern Adriatic domain aimed at constraining the geometry of the active faults deemed to be potential sources of moderate to large earthquakes in this region and at evaluating their long-term slip rates. This system of contractional structures is associated with fault-propagation folds outcropping along the coast or buried in the offshore that have been active at least since about 3Myr. The ongoing deformation of the coastal and offshore Marche thrust system is associated with moderate historical and instrumental seismicity and recorded in sedimentary and geomorphic features. In this study, we use subsurface data coming from both published and original sources. These comprise cross-sections, seismic lines, subsurface maps and borehole data to constrain geometrically coherent local 3D geological models, with particular focus on the Pliocene and Pleistocene units. Two sections crossing five main faults and correlative anticlines are extracted to calculate slip rates on the driving thrust faults. Our slip rate calculation procedure includes a) the assessment of the onset time which is based on the sedimentary and structural architecture, b) the decompaction of clastic units where necessary, and c) the restoration of the slip on the fault planes. The assessment of the differential compaction history of clastic rocks eliminates the effects of compaction-induced subsidence which determine unwanted overestimation of slip rates. To restore the displacement along the analyzed structures, we use two different methods on the basis of the deformation style: the fault parallel flow algorithm for faulted horizons and the trishear algorithm for fault-propagation folds. The time of fault onset ranges between 5.3-2.2 Myr; overall the average slip rates of the various thrusts are in the range of 0.26-1.35 mm/yr.en
dc.language.isoEnglishen
dc.publisher.nameElsevier Scienceen
dc.relation.ispartofMarine and petroleum geologyen
dc.relation.ispartofseries/42(2013)en
dc.subjectslip rateen
dc.subject3D geological modelen
dc.subjectstructural restorationen
dc.subjectseismogenic sourceen
dc.subjectthrust tectonicsen
dc.subjectnorthern Apenninesen
dc.subjectAdriatic Seaen
dc.titleDeriving thrust fault slip rates from geological modeling: examples from the Marche coastal and offshore contraction belt, Northern Apennines, Italy.en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber122-134en
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.04. Marine geologyen
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.09. Structural geologyen
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.04. Plate boundaries, motion, and tectonicsen
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonicsen
dc.identifier.doi10.1016/j.marpetgeo.2012.10.008en
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dc.description.obiettivoSpecifico3.2. Tettonica attivaen
dc.description.obiettivoSpecifico4.2. TTC - Modelli per la stima della pericolosità sismica a scala nazionaleen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.relation.issn0264-8172en
dc.relation.eissn1873-4073en
dc.contributor.authorMaesano, F. E.en
dc.contributor.authorToscani, G.en
dc.contributor.authorBurrato, P.en
dc.contributor.authorMirabella, F.en
dc.contributor.authorD'ambrogi, C.en
dc.contributor.authorBasili, R.en
dc.contributor.departmentDipartimento di Scienze della Terra e dell'Ambiente, Università di Paviaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentDipartimento di Scienze della Terra, Università di Perugiaen
dc.contributor.departmentISPRA - Servizio Geologico d'Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
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item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
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crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptDipartimento di Scienze della Terra, Università di Pavia. Via Ferrata, 1 - 27100 Pavia, Italy-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptUniversità degli Studi di Perugia-
crisitem.author.deptIstituto Superiore Protezione e Ricerca Ambientale-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.orcid0000-0002-5652-1548-
crisitem.author.orcid0000-0001-6588-7560-
crisitem.author.orcid0000-0002-1213-0828-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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