FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2316391324> ?p ?o ?g. }

• W2316391324 endingPage "254" @default.
• W2316391324 startingPage "251" @default.
• W2316391324 abstract "Research Article| March 01, 2012 Splay fault slip during the Mw 8.8 2010 Maule Chile earthquake Daniel Melnick; Daniel Melnick * 1Institut für Erd- und Umweltwissenschaften and DFG Leibniz Center for Surface Process and Climate Studies, Universität Potsdam, 14415 Potsdam, Germany *E-mail: melnick@geo.uni-potsdam.de. Search for other works by this author on: GSW Google Scholar Marcos Moreno; Marcos Moreno 2Deutsches GeoForschungsZentrum Potsdam, 14473 Potsdam, Germany Search for other works by this author on: GSW Google Scholar Mahdi Motagh; Mahdi Motagh 2Deutsches GeoForschungsZentrum Potsdam, 14473 Potsdam, Germany Search for other works by this author on: GSW Google Scholar Marco Cisternas; Marco Cisternas 3Escuela de Ciencias del Mar, Pontificia Universidad Católica de Valparaíso, 1020 Valparaíso, Chile Search for other works by this author on: GSW Google Scholar Robert L. Wesson Robert L. Wesson 4U.S. Geological Survey, Denver, Colorado 80225-0046, USA Search for other works by this author on: GSW Google Scholar Author and Article Information Daniel Melnick * 1Institut für Erd- und Umweltwissenschaften and DFG Leibniz Center for Surface Process and Climate Studies, Universität Potsdam, 14415 Potsdam, Germany Marcos Moreno 2Deutsches GeoForschungsZentrum Potsdam, 14473 Potsdam, Germany Mahdi Motagh 2Deutsches GeoForschungsZentrum Potsdam, 14473 Potsdam, Germany Marco Cisternas 3Escuela de Ciencias del Mar, Pontificia Universidad Católica de Valparaíso, 1020 Valparaíso, Chile Robert L. Wesson 4U.S. Geological Survey, Denver, Colorado 80225-0046, USA *E-mail: melnick@geo.uni-potsdam.de. Publisher: Geological Society of America Received: 07 Aug 2011 Revision Received: 12 Oct 2011 Accepted: 17 Oct 2011 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2012 Geological Society of America Geology (2012) 40 (3): 251–254. https://doi.org/10.1130/G32712.1 Article history Received: 07 Aug 2011 Revision Received: 12 Oct 2011 Accepted: 17 Oct 2011 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Daniel Melnick, Marcos Moreno, Mahdi Motagh, Marco Cisternas, Robert L. Wesson; Splay fault slip during the Mw 8.8 2010 Maule Chile earthquake. Geology 2012;; 40 (3): 251–254. doi: https://doi.org/10.1130/G32712.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Splay faults are thrusts that emerge from the plate boundaries of subduction zones. Such structures have been mapped at several convergent margins and their activity commonly ascribed to large megathrust earthquakes. However, the behavior of splay faults during the earthquake cycle is poorly constrained because typically these structures are located offshore and are difficult to access. Here we use geologic mapping combined with space and land geodesy, as well as offshore sonar data, to document surface-fault ruptures and coastal uplift at Isla Santa María in south-central Chile (37°S) caused by the 27 February 2010 Maule earthquake (Mw 8.8). During the earthquake, the island was tilted parallel to the margin, and normal faults ruptured the surface and adjacent ocean bottom. We associate tilt and crestal normal faulting with growth of an anticline above a blind reverse fault rooted in the Nazca–South America plate boundary, which slipped during the Maule earthquake. The splay fault system has formed in an area of reduced coseismic plate-boundary slip, suggesting that anelastic deformation in the upper plate may have restrained the 2010 megathrust rupture. Surface fault breaks were accompanied by prominent discharge of fluids. Our field observations support the notion that splay faulting may frequently complement and influence the rupture of subduction-zone earthquakes. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
• W2316391324 created "2016-06-24" @default.
• W2316391324 creator A5008770894 @default.
• W2316391324 creator A5017037499 @default.
• W2316391324 creator A5019551046 @default.
• W2316391324 creator A5070047836 @default.
• W2316391324 creator A5084320319 @default.
• W2316391324 date "2012-01-23" @default.
• W2316391324 modified "2023-10-17" @default.
• W2316391324 title "Splay fault slip during the Mw 8.8 2010 Maule Chile earthquake" @default.
• W2316391324 cites W1507372749 @default.
• W2316391324 cites W1537905573 @default.
• W2316391324 cites W1560829252 @default.
• W2316391324 cites W1570667357 @default.
• W2316391324 cites W1746069029 @default.
• W2316391324 cites W1840778637 @default.
• W2316391324 cites W1864564018 @default.
• W2316391324 cites W1967150943 @default.
• W2316391324 cites W1970303579 @default.
• W2316391324 cites W1975521649 @default.
• W2316391324 cites W1987800877 @default.
• W2316391324 cites W1988347634 @default.
• W2316391324 cites W1997576449 @default.
• W2316391324 cites W1998315724 @default.
• W2316391324 cites W2020996000 @default.
• W2316391324 cites W2030511467 @default.
• W2316391324 cites W2040407988 @default.
• W2316391324 cites W2040614796 @default.
• W2316391324 cites W2094395382 @default.
• W2316391324 cites W2107570727 @default.
• W2316391324 cites W2110381646 @default.
• W2316391324 cites W2136247519 @default.
• W2316391324 cites W2144667321 @default.
• W2316391324 cites W2150863356 @default.
• W2316391324 doi "https://doi.org/10.1130/g32712.1" @default.
• W2316391324 hasPublicationYear "2012" @default.
• W2316391324 type Work @default.
• W2316391324 sameAs 2316391324 @default.
• W2316391324 citedByCount "77" @default.
• W2316391324 countsByYear W23163913242012 @default.
• W2316391324 countsByYear W23163913242013 @default.
• W2316391324 countsByYear W23163913242014 @default.
• W2316391324 countsByYear W23163913242015 @default.
• W2316391324 countsByYear W23163913242016 @default.
• W2316391324 countsByYear W23163913242017 @default.
• W2316391324 countsByYear W23163913242018 @default.
• W2316391324 countsByYear W23163913242019 @default.
• W2316391324 countsByYear W23163913242020 @default.
• W2316391324 countsByYear W23163913242021 @default.
• W2316391324 countsByYear W23163913242022 @default.
• W2316391324 countsByYear W23163913242023 @default.
• W2316391324 crossrefType "journal-article" @default.
• W2316391324 hasAuthorship W2316391324A5008770894 @default.
• W2316391324 hasAuthorship W2316391324A5017037499 @default.
• W2316391324 hasAuthorship W2316391324A5019551046 @default.
• W2316391324 hasAuthorship W2316391324A5070047836 @default.
• W2316391324 hasAuthorship W2316391324A5084320319 @default.
• W2316391324 hasConcept C127313418 @default.
• W2316391324 hasConcept C142362112 @default.
• W2316391324 hasConcept C151730666 @default.
• W2316391324 hasConcept C15708023 @default.
• W2316391324 hasConcept C161191863 @default.
• W2316391324 hasConcept C2781113848 @default.
• W2316391324 hasConcept C41008148 @default.
• W2316391324 hasConceptScore W2316391324C127313418 @default.
• W2316391324 hasConceptScore W2316391324C142362112 @default.
• W2316391324 hasConceptScore W2316391324C151730666 @default.
• W2316391324 hasConceptScore W2316391324C15708023 @default.
• W2316391324 hasConceptScore W2316391324C161191863 @default.
• W2316391324 hasConceptScore W2316391324C2781113848 @default.
• W2316391324 hasConceptScore W2316391324C41008148 @default.
• W2316391324 hasIssue "3" @default.
• W2316391324 hasLocation W23163913241 @default.
• W2316391324 hasOpenAccess W2316391324 @default.
• W2316391324 hasPrimaryLocation W23163913241 @default.
• W2316391324 hasRelatedWork W1984402782 @default.
• W2316391324 hasRelatedWork W1999913942 @default.
• W2316391324 hasRelatedWork W2076393078 @default.
• W2316391324 hasRelatedWork W2086120259 @default.
• W2316391324 hasRelatedWork W2137941439 @default.
• W2316391324 hasRelatedWork W2151614148 @default.
• W2316391324 hasRelatedWork W2245170124 @default.
• W2316391324 hasRelatedWork W2324615561 @default.
• W2316391324 hasRelatedWork W2997386600 @default.
• W2316391324 hasRelatedWork W3186982001 @default.
• W2316391324 hasVolume "40" @default.
• W2316391324 isParatext "false" @default.
• W2316391324 isRetracted "false" @default.
• W2316391324 magId "2316391324" @default.
• W2316391324 workType "article" @default.