FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2071551683> ?p ?o ?g. }

• W2071551683 endingPage "823" @default.
• W2071551683 startingPage "811" @default.
• W2071551683 abstract "A new tectonic model reconciles conflicting structural and geochemical evidence for the origin of the Troodos ophiolite, a well‐preserved remnant of Neotethyan oceanic crust. Grabens and normal faults within the sheeted dike complex and the extrusive sequence of the Troodos ophiolite resemble those of oceanic spreading centers. Diverse intrusive and tectonic contact relationships between the sheeted dike complex and the underlying plutonic sequence indicate multiple and episodic intrusion of magma and along‐ and across‐strike variation in volcanic and tectonic activity during development of oceanic crust. Coupled with the existence of the Arakapas transform fault to the south, these structural and intrusive relationships suggest origin at an intersection between a spreading center and a transform fault. The arclike chemistry of sheeted dikes and related extrusive rocks and the inferred highly depleted and hydrous nature of the mantle source of the late stage intrusive and extrusive rocks argue, however, for generation of part of the ophiolite within a subduction zone environment. Regional reconstructions suggest that the Mesozoic Neotethys may have evolved as a marginal basin both to the Afro‐Arabian continent and the Paleotethyan ocean over an active or recently active south dipping subduction zone. The Troodos ophiolite and other eastern Mediterranean ophiolites, whose magma compositions were affected by the subducted Paleotethyan slab, may have formed along east‐west trending spreading centers separated by north‐south trending transform faults within this marginal basin. A rapid change in relative plate motion in late Cretaceous time between Eurasia and Afro‐Arabia created a regional compressive regime that may have resulted in plate boundary reorganizations within the Neotethyan realm and in initiation of north dipping subduction zone(s) beneath the Troodos and other ophiolites in the region. The apparent forearc setting of the Troodos ophiolite is a consequence of this intraoceanic displacement after its formation and thus is unrelated to its generation." @default.
• W2071551683 created "2016-06-24" @default.
• W2071551683 creator A5000607739 @default.
• W2071551683 creator A5025170650 @default.
• W2071551683 creator A5038138492 @default.
• W2071551683 creator A5045893170 @default.
• W2071551683 date "1990-08-01" @default.
• W2071551683 modified "2023-10-13" @default.
• W2071551683 title "Tectonic evolution of the Troodos Ophiolite within the Tethyan Framework" @default.
• W2071551683 cites W1964178171 @default.
• W2071551683 cites W1965808859 @default.
• W2071551683 cites W1971708279 @default.
• W2071551683 cites W1971808638 @default.
• W2071551683 cites W1988960219 @default.
• W2071551683 cites W1991091117 @default.
• W2071551683 cites W1994893680 @default.
• W2071551683 cites W1995815941 @default.
• W2071551683 cites W1999194663 @default.
• W2071551683 cites W2003866529 @default.
• W2071551683 cites W2004778581 @default.
• W2071551683 cites W2011268039 @default.
• W2071551683 cites W2019741248 @default.
• W2071551683 cites W2020551788 @default.
• W2071551683 cites W2032767312 @default.
• W2071551683 cites W2041176411 @default.
• W2071551683 cites W2041437561 @default.
• W2071551683 cites W2046829014 @default.
• W2071551683 cites W2047396493 @default.
• W2071551683 cites W2050577071 @default.
• W2071551683 cites W2053395903 @default.
• W2071551683 cites W2067897492 @default.
• W2071551683 cites W2075016059 @default.
• W2071551683 cites W2077049179 @default.
• W2071551683 cites W2078327345 @default.
• W2071551683 cites W2091485883 @default.
• W2071551683 cites W2098352994 @default.
• W2071551683 cites W2104837834 @default.
• W2071551683 cites W2109335656 @default.
• W2071551683 cites W2146649509 @default.
• W2071551683 cites W2149576353 @default.
• W2071551683 cites W2158363031 @default.
• W2071551683 cites W2168683587 @default.
• W2071551683 cites W2287722167 @default.
• W2071551683 cites W2904844428 @default.
• W2071551683 cites W4205749704 @default.
• W2071551683 doi "https://doi.org/10.1029/tc009i004p00811" @default.
• W2071551683 hasPublicationYear "1990" @default.
• W2071551683 type Work @default.
• W2071551683 sameAs 2071551683 @default.
• W2071551683 citedByCount "83" @default.
• W2071551683 countsByYear W20715516832012 @default.
• W2071551683 countsByYear W20715516832013 @default.
• W2071551683 countsByYear W20715516832014 @default.
• W2071551683 countsByYear W20715516832015 @default.
• W2071551683 countsByYear W20715516832018 @default.
• W2071551683 countsByYear W20715516832019 @default.
• W2071551683 countsByYear W20715516832020 @default.
• W2071551683 countsByYear W20715516832021 @default.
• W2071551683 countsByYear W20715516832022 @default.
• W2071551683 countsByYear W20715516832023 @default.
• W2071551683 crossrefType "journal-article" @default.
• W2071551683 hasAuthorship W2071551683A5000607739 @default.
• W2071551683 hasAuthorship W2071551683A5025170650 @default.
• W2071551683 hasAuthorship W2071551683A5038138492 @default.
• W2071551683 hasAuthorship W2071551683A5045893170 @default.
• W2071551683 hasConcept C106973953 @default.
• W2071551683 hasConcept C119477230 @default.
• W2071551683 hasConcept C120806208 @default.
• W2071551683 hasConcept C127313418 @default.
• W2071551683 hasConcept C151730666 @default.
• W2071551683 hasConcept C154200439 @default.
• W2071551683 hasConcept C17409809 @default.
• W2071551683 hasConcept C192241223 @default.
• W2071551683 hasConcept C193944797 @default.
• W2071551683 hasConcept C1965285 @default.
• W2071551683 hasConcept C23923706 @default.
• W2071551683 hasConcept C2776698055 @default.
• W2071551683 hasConcept C58097730 @default.
• W2071551683 hasConcept C77928131 @default.
• W2071551683 hasConcept C83893233 @default.
• W2071551683 hasConceptScore W2071551683C106973953 @default.
• W2071551683 hasConceptScore W2071551683C119477230 @default.
• W2071551683 hasConceptScore W2071551683C120806208 @default.
• W2071551683 hasConceptScore W2071551683C127313418 @default.
• W2071551683 hasConceptScore W2071551683C151730666 @default.
• W2071551683 hasConceptScore W2071551683C154200439 @default.
• W2071551683 hasConceptScore W2071551683C17409809 @default.
• W2071551683 hasConceptScore W2071551683C192241223 @default.
• W2071551683 hasConceptScore W2071551683C193944797 @default.
• W2071551683 hasConceptScore W2071551683C1965285 @default.
• W2071551683 hasConceptScore W2071551683C23923706 @default.
• W2071551683 hasConceptScore W2071551683C2776698055 @default.
• W2071551683 hasConceptScore W2071551683C58097730 @default.
• W2071551683 hasConceptScore W2071551683C77928131 @default.
• W2071551683 hasConceptScore W2071551683C83893233 @default.
• W2071551683 hasIssue "4" @default.
• W2071551683 hasLocation W20715516831 @default.
• W2071551683 hasOpenAccess W2071551683 @default.

• next