FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1978795897> ?p ?o ?g. }

• W1978795897 endingPage "100" @default.
• W1978795897 startingPage "93" @default.
• W1978795897 abstract "Research Article| April 01, 2014 Ophiolites and Their Origins Yildirim Dilek; Yildirim Dilek 1Department of Geology & Environmental Earth Science, Miami University, Oxford, OH 45056, USAE-mail: dileky@miamioh.edu Search for other works by this author on: GSW Google Scholar Harald Furnes Harald Furnes 2Department of Earth Science & Centre for Geobiology, University of Bergen, 5007 Bergen, Norway Search for other works by this author on: GSW Google Scholar Elements (2014) 10 (2): 93–100. https://doi.org/10.2113/gselements.10.2.93 Article history first online: 09 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 Yildirim Dilek, Harald Furnes; Ophiolites and Their Origins. Elements 2014;; 10 (2): 93–100. doi: https://doi.org/10.2113/gselements.10.2.93 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 SocietyElements Search Advanced Search Abstract Ophiolites are suites of temporally and spatially associated ultramafic, mafic, and felsic rocks that are interpreted to be remnants of ancient oceanic crust and upper mantle. Ophiolites show significant variations in their internal structure, geochemical fingerprints, and emplacement mechanisms. These differences are controlled by (1) the proximity, when formed at the magmatic stage, to a plume or trench; (2) the rate, geometry, and nature of ocean-ridge spreading; (3) mantle composition, temperature, and fertility; and (4) the availability of fluids. The oceanic crust preserved in ophiolites may form in any tectonic setting during the evolution of ocean basins, from the rift–drift and seafloor spreading stages to subduction initiation and terminal closure. An ophiolite is emplaced either from downgoing oceanic lithosphere via subduction-accretion or from the upper plate in a subduction zone through trench–continent collision. Subduction zone tectonics is thus the most important factor in the igneous evolution of ophiolites and their emplacement into continental margins. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
• W1978795897 created "2016-06-24" @default.
• W1978795897 creator A5045811783 @default.
• W1978795897 creator A5084944585 @default.
• W1978795897 date "2014-04-01" @default.
• W1978795897 modified "2023-10-16" @default.
• W1978795897 title "Ophiolites and Their Origins" @default.
• W1978795897 cites W1669936631 @default.
• W1978795897 cites W1966172018 @default.
• W1978795897 cites W1967579043 @default.
• W1978795897 cites W1969845853 @default.
• W1978795897 cites W1984883209 @default.
• W1978795897 cites W2003323528 @default.
• W1978795897 cites W2008531647 @default.
• W1978795897 cites W2017840788 @default.
• W1978795897 cites W2018172800 @default.
• W1978795897 cites W2032763493 @default.
• W1978795897 cites W2042806383 @default.
• W1978795897 cites W2045859284 @default.
• W1978795897 cites W2047396493 @default.
• W1978795897 cites W2047519592 @default.
• W1978795897 cites W2052690035 @default.
• W1978795897 cites W2073878298 @default.
• W1978795897 cites W2079376467 @default.
• W1978795897 cites W2083395736 @default.
• W1978795897 cites W2086820683 @default.
• W1978795897 cites W2119056569 @default.
• W1978795897 cites W2121537280 @default.
• W1978795897 cites W2135595445 @default.
• W1978795897 cites W2141567058 @default.
• W1978795897 cites W2156744603 @default.
• W1978795897 cites W2161493148 @default.
• W1978795897 cites W220644591 @default.
• W1978795897 cites W2312828419 @default.
• W1978795897 cites W2317691790 @default.
• W1978795897 cites W2320975253 @default.
• W1978795897 cites W2337692353 @default.
• W1978795897 cites W3112908339 @default.
• W1978795897 doi "https://doi.org/10.2113/gselements.10.2.93" @default.
• W1978795897 hasPublicationYear "2014" @default.
• W1978795897 type Work @default.
• W1978795897 sameAs 1978795897 @default.
• W1978795897 citedByCount "469" @default.
• W1978795897 countsByYear W19787958972014 @default.
• W1978795897 countsByYear W19787958972015 @default.
• W1978795897 countsByYear W19787958972016 @default.
• W1978795897 countsByYear W19787958972017 @default.
• W1978795897 countsByYear W19787958972018 @default.
• W1978795897 countsByYear W19787958972019 @default.
• W1978795897 countsByYear W19787958972020 @default.
• W1978795897 countsByYear W19787958972021 @default.
• W1978795897 countsByYear W19787958972022 @default.
• W1978795897 countsByYear W19787958972023 @default.
• W1978795897 crossrefType "journal-article" @default.
• W1978795897 hasAuthorship W1978795897A5045811783 @default.
• W1978795897 hasAuthorship W1978795897A5084944585 @default.
• W1978795897 hasConcept C127313418 @default.
• W1978795897 hasConcept C151730666 @default.
• W1978795897 hasConcept C17409809 @default.
• W1978795897 hasConcept C1965285 @default.
• W1978795897 hasConcept C199360897 @default.
• W1978795897 hasConcept C23923706 @default.
• W1978795897 hasConcept C2778447006 @default.
• W1978795897 hasConcept C41008148 @default.
• W1978795897 hasConcept C77928131 @default.
• W1978795897 hasConceptScore W1978795897C127313418 @default.
• W1978795897 hasConceptScore W1978795897C151730666 @default.
• W1978795897 hasConceptScore W1978795897C17409809 @default.
• W1978795897 hasConceptScore W1978795897C1965285 @default.
• W1978795897 hasConceptScore W1978795897C199360897 @default.
• W1978795897 hasConceptScore W1978795897C23923706 @default.
• W1978795897 hasConceptScore W1978795897C2778447006 @default.
• W1978795897 hasConceptScore W1978795897C41008148 @default.
• W1978795897 hasConceptScore W1978795897C77928131 @default.
• W1978795897 hasIssue "2" @default.
• W1978795897 hasLocation W19787958971 @default.
• W1978795897 hasOpenAccess W1978795897 @default.
• W1978795897 hasPrimaryLocation W19787958971 @default.
• W1978795897 hasRelatedWork W1996887763 @default.
• W1978795897 hasRelatedWork W2009501387 @default.
• W1978795897 hasRelatedWork W2028167649 @default.
• W1978795897 hasRelatedWork W2059524392 @default.
• W1978795897 hasRelatedWork W2070061059 @default.
• W1978795897 hasRelatedWork W2092489160 @default.
• W1978795897 hasRelatedWork W2160719201 @default.
• W1978795897 hasRelatedWork W2286592209 @default.
• W1978795897 hasRelatedWork W2375924447 @default.
• W1978795897 hasRelatedWork W2392013236 @default.
• W1978795897 hasVolume "10" @default.
• W1978795897 isParatext "false" @default.
• W1978795897 isRetracted "false" @default.
• W1978795897 magId "1978795897" @default.
• W1978795897 workType "article" @default.