FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2045856740> ?p ?o ?g. }

• W2045856740 endingPage "422" @default.
• W2045856740 startingPage "419" @default.
• W2045856740 abstract "Research Article| May 01, 2009 Downdip segmentation of strike-slip fault zones in the brittle crust Eliza S. Nemser; Eliza S. Nemser 1Department of Earth and Space Sciences, University of Washington, Seattle, Washington 98195-1310, USA Search for other works by this author on: GSW Google Scholar Darrel S. Cowan Darrel S. Cowan 1Department of Earth and Space Sciences, University of Washington, Seattle, Washington 98195-1310, USA Search for other works by this author on: GSW Google Scholar Geology (2009) 37 (5): 419–422. https://doi.org/10.1130/G25619A.1 Article history received: 21 Oct 2008 rev-recd: 11 Dec 2008 accepted: 16 Dec 2008 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Eliza S. Nemser, Darrel S. Cowan; Downdip segmentation of strike-slip fault zones in the brittle crust. Geology 2009;; 37 (5): 419–422. doi: https://doi.org/10.1130/G25619A.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 Outcrop-scale field evidence from the southern San Jacinto fault zone in southern California indicates that bedding-parallel slip may be an important mechanism for transferring and accommodating slip within strike-slip fault zones that cut across heterogeneous stratigraphy. Steeply dipping strike-slip fault segments exposed in conglomeratic sandstones abruptly terminate at weaker shale layers where slip occurs on bedding-parallel planes. Cross sections of fault-related seismicity within the southern San Jacinto fault zone reveal that events generally cluster within tabular, steeply dipping fault-parallel streaks that are limited in extent in the downdip direction. The depths of the downdip terminations of shallow streaks tend to be roughly coincident with the depths of the updip terminations of deeper streaks; these configurations define stepover geometries that range in character from sharp to diffuse. The examples described herein provide evidence that downdip segmentation within strike-slip fault zones may be common over a wide range of scales. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
• W2045856740 created "2016-06-24" @default.
• W2045856740 creator A5010844483 @default.
• W2045856740 creator A5062631281 @default.
• W2045856740 date "2009-05-01" @default.
• W2045856740 modified "2023-09-30" @default.
• W2045856740 title "Downdip segmentation of strike-slip fault zones in the brittle crust" @default.
• W2045856740 cites W1486980017 @default.
• W2045856740 cites W1976435903 @default.
• W2045856740 cites W1988818557 @default.
• W2045856740 cites W1989007517 @default.
• W2045856740 cites W1990893288 @default.
• W2045856740 cites W2002912307 @default.
• W2045856740 cites W2038388062 @default.
• W2045856740 cites W2046902020 @default.
• W2045856740 cites W2047957907 @default.
• W2045856740 cites W2052369031 @default.
• W2045856740 cites W2068880412 @default.
• W2045856740 cites W2071821532 @default.
• W2045856740 cites W2079677265 @default.
• W2045856740 cites W2093201898 @default.
• W2045856740 cites W2097057329 @default.
• W2045856740 cites W2141594790 @default.
• W2045856740 cites W2147222936 @default.
• W2045856740 cites W2151476010 @default.
• W2045856740 cites W2167750495 @default.
• W2045856740 cites W2171375152 @default.
• W2045856740 doi "https://doi.org/10.1130/g25619a.1" @default.
• W2045856740 hasPublicationYear "2009" @default.
• W2045856740 type Work @default.
• W2045856740 sameAs 2045856740 @default.
• W2045856740 citedByCount "11" @default.
• W2045856740 countsByYear W20458567402013 @default.
• W2045856740 countsByYear W20458567402014 @default.
• W2045856740 countsByYear W20458567402015 @default.
• W2045856740 countsByYear W20458567402017 @default.
• W2045856740 countsByYear W20458567402019 @default.
• W2045856740 countsByYear W20458567402023 @default.
• W2045856740 crossrefType "journal-article" @default.
• W2045856740 hasAuthorship W2045856740A5010844483 @default.
• W2045856740 hasAuthorship W2045856740A5062631281 @default.
• W2045856740 hasConcept C127313418 @default.
• W2045856740 hasConcept C127413603 @default.
• W2045856740 hasConcept C146978453 @default.
• W2045856740 hasConcept C151730666 @default.
• W2045856740 hasConcept C161191863 @default.
• W2045856740 hasConcept C165205528 @default.
• W2045856740 hasConcept C169212394 @default.
• W2045856740 hasConcept C195268267 @default.
• W2045856740 hasConcept C199360897 @default.
• W2045856740 hasConcept C2776698055 @default.
• W2045856740 hasConcept C2778447006 @default.
• W2045856740 hasConcept C2778805511 @default.
• W2045856740 hasConcept C41008148 @default.
• W2045856740 hasConceptScore W2045856740C127313418 @default.
• W2045856740 hasConceptScore W2045856740C127413603 @default.
• W2045856740 hasConceptScore W2045856740C146978453 @default.
• W2045856740 hasConceptScore W2045856740C151730666 @default.
• W2045856740 hasConceptScore W2045856740C161191863 @default.
• W2045856740 hasConceptScore W2045856740C165205528 @default.
• W2045856740 hasConceptScore W2045856740C169212394 @default.
• W2045856740 hasConceptScore W2045856740C195268267 @default.
• W2045856740 hasConceptScore W2045856740C199360897 @default.
• W2045856740 hasConceptScore W2045856740C2776698055 @default.
• W2045856740 hasConceptScore W2045856740C2778447006 @default.
• W2045856740 hasConceptScore W2045856740C2778805511 @default.
• W2045856740 hasConceptScore W2045856740C41008148 @default.
• W2045856740 hasIssue "5" @default.
• W2045856740 hasLocation W20458567401 @default.
• W2045856740 hasOpenAccess W2045856740 @default.
• W2045856740 hasPrimaryLocation W20458567401 @default.
• W2045856740 hasRelatedWork W1975776582 @default.
• W2045856740 hasRelatedWork W2056111981 @default.
• W2045856740 hasRelatedWork W2087614875 @default.
• W2045856740 hasRelatedWork W2105401011 @default.
• W2045856740 hasRelatedWork W2126425139 @default.
• W2045856740 hasRelatedWork W2135101066 @default.
• W2045856740 hasRelatedWork W2146831427 @default.
• W2045856740 hasRelatedWork W2155281179 @default.
• W2045856740 hasRelatedWork W2794856591 @default.
• W2045856740 hasRelatedWork W2798082128 @default.
• W2045856740 hasVolume "37" @default.
• W2045856740 isParatext "false" @default.
• W2045856740 isRetracted "false" @default.
• W2045856740 magId "2045856740" @default.
• W2045856740 workType "article" @default.