FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2010146361> ?p ?o ?g. }

• W2010146361 endingPage "617" @default.
• W2010146361 startingPage "617" @default.
• W2010146361 abstract "Research Article| July 01, 2004 Long-term subduction-erosion along the Guatemalan margin of the Middle America Trench Paola Vannucchi; Paola Vannucchi 1Dipartimento di Scienze della Terra, Università di Firenze, Via La Pira, 4, 50121 Firenze, Italy Search for other works by this author on: GSW Google Scholar Simone Galeotti; Simone Galeotti 2Istituto di Geologia, Università di Urbino, Località Crocicchia, 61029 Urbino, Italy Search for other works by this author on: GSW Google Scholar Peter D. Clift; Peter D. Clift 3Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA Search for other works by this author on: GSW Google Scholar César R. Ranero; César R. Ranero 4Institut für Meereswissenschaften, Research Center for Marine Geosciences, and Sonderforschungsbereich 574, Wischhofstrasse 1-3, 24148 Kiel, Germany Search for other works by this author on: GSW Google Scholar Roland von Huene Roland von Huene 5Department of Geology, University of California, Davis, California 95616, USA Search for other works by this author on: GSW Google Scholar Author and Article Information Paola Vannucchi 1Dipartimento di Scienze della Terra, Università di Firenze, Via La Pira, 4, 50121 Firenze, Italy Simone Galeotti 2Istituto di Geologia, Università di Urbino, Località Crocicchia, 61029 Urbino, Italy Peter D. Clift 3Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA César R. Ranero 4Institut für Meereswissenschaften, Research Center for Marine Geosciences, and Sonderforschungsbereich 574, Wischhofstrasse 1-3, 24148 Kiel, Germany Roland von Huene 5Department of Geology, University of California, Davis, California 95616, USA Publisher: Geological Society of America Received: 24 Dec 2003 Revision Received: 06 Mar 2004 Accepted: 11 Mar 2004 First Online: 02 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (2004) 32 (7): 617–620. https://doi.org/10.1130/G20422.1 Article history Received: 24 Dec 2003 Revision Received: 06 Mar 2004 Accepted: 11 Mar 2004 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Paola Vannucchi, Simone Galeotti, Peter D. Clift, César R. Ranero, Roland von Huene; Long-term subduction-erosion along the Guatemalan margin of the Middle America Trench. Geology 2004;; 32 (7): 617–620. doi: https://doi.org/10.1130/G20422.1 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 A new analysis of Deep Sea Drilling Project (DSDP) Leg 84 data demonstrates that the dominant process controlling the Guatemala margin tectonic evolution since ca. 25 Ma is subduction-erosion. Data from benthic foraminifera, assemblages from upper-slope DSDP Sites 568, 569, and 570 indicate long-term, progressive subsidence from upper to middle bathyal depths (600–1000 m) ca. 19 Ma to modern abyssal depths (>2000 m). Rapid subsidence migrated landward starting at the Oligocene-Miocene boundary time under the current middle slope, where it increased sharply ca. 19 Ma, reached the current upper slope by ca. 15 Ma, and arrived at the uppermost slope ca. 2 Ma. Subsidence indicates crustal thinning by basal tectonic erosion of mass from the underside of the upper plate. Under the assumption that, in the Miocene, the morphology of the forearc was similar to that of today, landward migration of the trench was at a rate of 0.8–0.9 km/m.y. This linear rate corresponds to a tectonic erosion rate of the submerged forearc of 11.3–13.1 km3·m.y.−1·km−1. The evolution of arc magmatism and superfast spreading at the East Pacific Rise since early Miocene time may have caused slab shallowing and tectonic erosion that readjusted the forearc geometry. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
• W2010146361 created "2016-06-24" @default.
• W2010146361 creator A5026388898 @default.
• W2010146361 creator A5039268898 @default.
• W2010146361 creator A5051201637 @default.
• W2010146361 creator A5058131929 @default.
• W2010146361 creator A5074170419 @default.
• W2010146361 date "2004-01-01" @default.
• W2010146361 modified "2023-10-02" @default.
• W2010146361 title "Long-term subduction-erosion along the Guatemalan margin of the Middle America Trench" @default.
• W2010146361 cites W1671207528 @default.
• W2010146361 cites W1966963411 @default.
• W2010146361 cites W1973739295 @default.
• W2010146361 cites W1978213839 @default.
• W2010146361 cites W1978465122 @default.
• W2010146361 cites W1997252211 @default.
• W2010146361 cites W2007237868 @default.
• W2010146361 cites W2016121206 @default.
• W2010146361 cites W2016737438 @default.
• W2010146361 cites W2030800261 @default.
• W2010146361 cites W2050426592 @default.
• W2010146361 cites W2064295076 @default.
• W2010146361 cites W2068495563 @default.
• W2010146361 cites W2093835541 @default.
• W2010146361 cites W2110585121 @default.
• W2010146361 cites W2142230665 @default.
• W2010146361 doi "https://doi.org/10.1130/g20422.1" @default.
• W2010146361 hasPublicationYear "2004" @default.
• W2010146361 type Work @default.
• W2010146361 sameAs 2010146361 @default.
• W2010146361 citedByCount "73" @default.
• W2010146361 countsByYear W20101463612012 @default.
• W2010146361 countsByYear W20101463612013 @default.
• W2010146361 countsByYear W20101463612014 @default.
• W2010146361 countsByYear W20101463612015 @default.
• W2010146361 countsByYear W20101463612016 @default.
• W2010146361 countsByYear W20101463612017 @default.
• W2010146361 countsByYear W20101463612018 @default.
• W2010146361 countsByYear W20101463612019 @default.
• W2010146361 countsByYear W20101463612020 @default.
• W2010146361 countsByYear W20101463612021 @default.
• W2010146361 countsByYear W20101463612022 @default.
• W2010146361 crossrefType "journal-article" @default.
• W2010146361 hasAuthorship W2010146361A5026388898 @default.
• W2010146361 hasAuthorship W2010146361A5039268898 @default.
• W2010146361 hasAuthorship W2010146361A5051201637 @default.
• W2010146361 hasAuthorship W2010146361A5058131929 @default.
• W2010146361 hasAuthorship W2010146361A5074170419 @default.
• W2010146361 hasBestOaLocation W20101463612 @default.
• W2010146361 hasConcept C127313418 @default.
• W2010146361 hasConcept C155310634 @default.
• W2010146361 hasConcept C165205528 @default.
• W2010146361 hasConcept C166957645 @default.
• W2010146361 hasConcept C178790620 @default.
• W2010146361 hasConcept C185592680 @default.
• W2010146361 hasConcept C2779227376 @default.
• W2010146361 hasConcept C58097730 @default.
• W2010146361 hasConcept C77928131 @default.
• W2010146361 hasConcept C95457728 @default.
• W2010146361 hasConceptScore W2010146361C127313418 @default.
• W2010146361 hasConceptScore W2010146361C155310634 @default.
• W2010146361 hasConceptScore W2010146361C165205528 @default.
• W2010146361 hasConceptScore W2010146361C166957645 @default.
• W2010146361 hasConceptScore W2010146361C178790620 @default.
• W2010146361 hasConceptScore W2010146361C185592680 @default.
• W2010146361 hasConceptScore W2010146361C2779227376 @default.
• W2010146361 hasConceptScore W2010146361C58097730 @default.
• W2010146361 hasConceptScore W2010146361C77928131 @default.
• W2010146361 hasConceptScore W2010146361C95457728 @default.
• W2010146361 hasIssue "7" @default.
• W2010146361 hasLocation W20101463611 @default.
• W2010146361 hasLocation W20101463612 @default.
• W2010146361 hasLocation W20101463613 @default.
• W2010146361 hasOpenAccess W2010146361 @default.
• W2010146361 hasPrimaryLocation W20101463611 @default.
• W2010146361 hasRelatedWork W1535852234 @default.
• W2010146361 hasRelatedWork W1922306407 @default.
• W2010146361 hasRelatedWork W2006773183 @default.
• W2010146361 hasRelatedWork W2026822772 @default.
• W2010146361 hasRelatedWork W2107520839 @default.
• W2010146361 hasRelatedWork W2127691210 @default.
• W2010146361 hasRelatedWork W2315564386 @default.
• W2010146361 hasRelatedWork W2604251004 @default.
• W2010146361 hasRelatedWork W3011208781 @default.
• W2010146361 hasRelatedWork W4386088354 @default.
• W2010146361 hasVolume "32" @default.
• W2010146361 isParatext "false" @default.
• W2010146361 isRetracted "false" @default.
• W2010146361 magId "2010146361" @default.
• W2010146361 workType "article" @default.