Matches in SemOpenAlex for { <https://semopenalex.org/work/W2067395633> ?p ?o ?g. }
- W2067395633 endingPage "134" @default.
- W2067395633 startingPage "122" @default.
- W2067395633 abstract "We 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 3 Myr. 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 and 2.2 Myr; overall the average slip rates of the various thrusts are in the range of 0.26–1.35 mm/yr." @default.
- W2067395633 created "2016-06-24" @default.
- W2067395633 creator A5008027026 @default.
- W2067395633 creator A5018396399 @default.
- W2067395633 creator A5024745999 @default.
- W2067395633 creator A5030193599 @default.
- W2067395633 creator A5037614386 @default.
- W2067395633 creator A5073604061 @default.
- W2067395633 date "2013-04-01" @default.
- W2067395633 modified "2023-10-13" @default.
- W2067395633 title "Deriving thrust fault slip rates from geological modeling: Examples from the Marche coastal and offshore contraction belt, Northern Apennines, Italy" @default.
- W2067395633 cites W1561405154 @default.
- W2067395633 cites W1614595254 @default.
- W2067395633 cites W1908251223 @default.
- W2067395633 cites W1969732380 @default.
- W2067395633 cites W1987277116 @default.
- W2067395633 cites W1989803896 @default.
- W2067395633 cites W1991826684 @default.
- W2067395633 cites W1992822549 @default.
- W2067395633 cites W1995764164 @default.
- W2067395633 cites W2004583345 @default.
- W2067395633 cites W2010602328 @default.
- W2067395633 cites W2033493316 @default.
- W2067395633 cites W2035113065 @default.
- W2067395633 cites W2038582040 @default.
- W2067395633 cites W2040999936 @default.
- W2067395633 cites W204449338 @default.
- W2067395633 cites W2060650057 @default.
- W2067395633 cites W2063342340 @default.
- W2067395633 cites W2064158161 @default.
- W2067395633 cites W2069919440 @default.
- W2067395633 cites W2082150282 @default.
- W2067395633 cites W2088664992 @default.
- W2067395633 cites W2093004440 @default.
- W2067395633 cites W2093184513 @default.
- W2067395633 cites W2095553002 @default.
- W2067395633 cites W2110585121 @default.
- W2067395633 cites W2119248594 @default.
- W2067395633 cites W2124426182 @default.
- W2067395633 cites W2125217075 @default.
- W2067395633 cites W2132926881 @default.
- W2067395633 cites W2148135691 @default.
- W2067395633 cites W2164873249 @default.
- W2067395633 cites W2165746064 @default.
- W2067395633 cites W2167194989 @default.
- W2067395633 cites W2172002706 @default.
- W2067395633 cites W2974031284 @default.
- W2067395633 cites W566089906 @default.
- W2067395633 doi "https://doi.org/10.1016/j.marpetgeo.2012.10.008" @default.
- W2067395633 hasPublicationYear "2013" @default.
- W2067395633 type Work @default.
- W2067395633 sameAs 2067395633 @default.
- W2067395633 citedByCount "42" @default.
- W2067395633 countsByYear W20673956332013 @default.
- W2067395633 countsByYear W20673956332014 @default.
- W2067395633 countsByYear W20673956332015 @default.
- W2067395633 countsByYear W20673956332016 @default.
- W2067395633 countsByYear W20673956332017 @default.
- W2067395633 countsByYear W20673956332019 @default.
- W2067395633 countsByYear W20673956332020 @default.
- W2067395633 countsByYear W20673956332021 @default.
- W2067395633 countsByYear W20673956332022 @default.
- W2067395633 countsByYear W20673956332023 @default.
- W2067395633 crossrefType "journal-article" @default.
- W2067395633 hasAuthorship W2067395633A5008027026 @default.
- W2067395633 hasAuthorship W2067395633A5018396399 @default.
- W2067395633 hasAuthorship W2067395633A5024745999 @default.
- W2067395633 hasAuthorship W2067395633A5030193599 @default.
- W2067395633 hasAuthorship W2067395633A5037614386 @default.
- W2067395633 hasAuthorship W2067395633A5073604061 @default.
- W2067395633 hasConcept C110041135 @default.
- W2067395633 hasConcept C116637073 @default.
- W2067395633 hasConcept C121332964 @default.
- W2067395633 hasConcept C127313418 @default.
- W2067395633 hasConcept C151730666 @default.
- W2067395633 hasConcept C162284963 @default.
- W2067395633 hasConcept C165205528 @default.
- W2067395633 hasConcept C175551986 @default.
- W2067395633 hasConcept C187320778 @default.
- W2067395633 hasConcept C195268267 @default.
- W2067395633 hasConcept C57803568 @default.
- W2067395633 hasConcept C6494504 @default.
- W2067395633 hasConcept C77928131 @default.
- W2067395633 hasConcept C97355855 @default.
- W2067395633 hasConceptScore W2067395633C110041135 @default.
- W2067395633 hasConceptScore W2067395633C116637073 @default.
- W2067395633 hasConceptScore W2067395633C121332964 @default.
- W2067395633 hasConceptScore W2067395633C127313418 @default.
- W2067395633 hasConceptScore W2067395633C151730666 @default.
- W2067395633 hasConceptScore W2067395633C162284963 @default.
- W2067395633 hasConceptScore W2067395633C165205528 @default.
- W2067395633 hasConceptScore W2067395633C175551986 @default.
- W2067395633 hasConceptScore W2067395633C187320778 @default.
- W2067395633 hasConceptScore W2067395633C195268267 @default.
- W2067395633 hasConceptScore W2067395633C57803568 @default.
- W2067395633 hasConceptScore W2067395633C6494504 @default.
- W2067395633 hasConceptScore W2067395633C77928131 @default.
- W2067395633 hasConceptScore W2067395633C97355855 @default.