FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2076636650> ?p ?o ?g. }

• W2076636650 endingPage "12" @default.
• W2076636650 startingPage "1" @default.
• W2076636650 abstract "Quaternary basaltic and andesitic lavas from the NW Iran/eastern Turkey border area are related to the active Arabia–Eurasia collision. The lavas occur within the Turkish–Iranian plateau, which ceased crustal thickening before the establishment of a number of volcanic centres within Iran and eastern Turkey, beginning at ~ 10 Ma. Models for generating syn-collision magmatism in eastern Anatolia have invoked slab-break-off beneath the thick crust and thin mantle lithosphere of the Cenozoic East Anatolia Accretionary Complex and/or partial loss of the lower lithosphere. Here we report geochemical and Sm–Nd/Rb–Sr data from a ~ 200 km long, N–S traverse that samples volcanic flows in NW Iran, many of which originate from centres in Turkey such as Ararat and Tendurek. Samples are transitional alkali/tholeiitic basalts and andesites. Ararat samples have lower Nb, lower large ion lithophile element (LILE) concentrations with 143Nd/144Nd ~ 0.51290. Other, volumetrically smaller, centres have higher Nb, higher LILE, with 143Nd/144Nd ~ 0.51265. Abundances of LILE and Nb increase from north to south. The presumed degree of partial melting increases in the opposite direction, away from the Arabia–Eurasia suture. Melting is inferred to have taken place in the spinel lherzolite field, largely from a continental lithosphere source influenced by Mesozoic and early Cenozoic Neo-Tethyan subduction, but a separate source with long-term enrichment is needed to explain the high Nb, lower 143Nd/144Nd compositions." @default.
• W2076636650 created "2016-06-24" @default.
• W2076636650 creator A5006655984 @default.
• W2076636650 creator A5019299931 @default.
• W2076636650 creator A5052313124 @default.
• W2076636650 date "2009-05-01" @default.
• W2076636650 modified "2023-10-01" @default.
• W2076636650 title "Quaternary syn-collision magmatism from the Iran/Turkey borderlands" @default.
• W2076636650 cites W1622026908 @default.
• W2076636650 cites W1967798189 @default.
• W2076636650 cites W1976630555 @default.
• W2076636650 cites W1979407478 @default.
• W2076636650 cites W1983690325 @default.
• W2076636650 cites W1986996860 @default.
• W2076636650 cites W1992736932 @default.
• W2076636650 cites W2003948785 @default.
• W2076636650 cites W2022061975 @default.
• W2076636650 cites W2028583699 @default.
• W2076636650 cites W2036884486 @default.
• W2076636650 cites W2041836270 @default.
• W2076636650 cites W2042360625 @default.
• W2076636650 cites W2043130905 @default.
• W2076636650 cites W2054578927 @default.
• W2076636650 cites W2058988888 @default.
• W2076636650 cites W2076735142 @default.
• W2076636650 cites W2079994847 @default.
• W2076636650 cites W2083465209 @default.
• W2076636650 cites W2102453637 @default.
• W2076636650 cites W2109596691 @default.
• W2076636650 cites W2131924853 @default.
• W2076636650 cites W2134736347 @default.
• W2076636650 cites W2135952135 @default.
• W2076636650 cites W2140554512 @default.
• W2076636650 cites W2145972115 @default.
• W2076636650 cites W2149175560 @default.
• W2076636650 cites W2171135774 @default.
• W2076636650 doi "https://doi.org/10.1016/j.jvolgeores.2009.01.026" @default.
• W2076636650 hasPublicationYear "2009" @default.
• W2076636650 type Work @default.
• W2076636650 sameAs 2076636650 @default.
• W2076636650 citedByCount "87" @default.
• W2076636650 countsByYear W20766366502012 @default.
• W2076636650 countsByYear W20766366502013 @default.
• W2076636650 countsByYear W20766366502014 @default.
• W2076636650 countsByYear W20766366502015 @default.
• W2076636650 countsByYear W20766366502016 @default.
• W2076636650 countsByYear W20766366502017 @default.
• W2076636650 countsByYear W20766366502018 @default.
• W2076636650 countsByYear W20766366502019 @default.
• W2076636650 countsByYear W20766366502020 @default.
• W2076636650 countsByYear W20766366502021 @default.
• W2076636650 countsByYear W20766366502022 @default.
• W2076636650 countsByYear W20766366502023 @default.
• W2076636650 crossrefType "journal-article" @default.
• W2076636650 hasAuthorship W2076636650A5006655984 @default.
• W2076636650 hasAuthorship W2076636650A5019299931 @default.
• W2076636650 hasAuthorship W2076636650A5052313124 @default.
• W2076636650 hasBestOaLocation W20766366502 @default.
• W2076636650 hasConcept C121704057 @default.
• W2076636650 hasConcept C127313418 @default.
• W2076636650 hasConcept C151730666 @default.
• W2076636650 hasConcept C160464908 @default.
• W2076636650 hasConcept C162973429 @default.
• W2076636650 hasConcept C165205528 @default.
• W2076636650 hasConcept C17409809 @default.
• W2076636650 hasConcept C38652104 @default.
• W2076636650 hasConcept C41008148 @default.
• W2076636650 hasConcept C77928131 @default.
• W2076636650 hasConceptScore W2076636650C121704057 @default.
• W2076636650 hasConceptScore W2076636650C127313418 @default.
• W2076636650 hasConceptScore W2076636650C151730666 @default.
• W2076636650 hasConceptScore W2076636650C160464908 @default.
• W2076636650 hasConceptScore W2076636650C162973429 @default.
• W2076636650 hasConceptScore W2076636650C165205528 @default.
• W2076636650 hasConceptScore W2076636650C17409809 @default.
• W2076636650 hasConceptScore W2076636650C38652104 @default.
• W2076636650 hasConceptScore W2076636650C41008148 @default.
• W2076636650 hasConceptScore W2076636650C77928131 @default.
• W2076636650 hasIssue "1-2" @default.
• W2076636650 hasLocation W20766366501 @default.
• W2076636650 hasLocation W20766366502 @default.
• W2076636650 hasLocation W20766366503 @default.
• W2076636650 hasOpenAccess W2076636650 @default.
• W2076636650 hasPrimaryLocation W20766366501 @default.
• W2076636650 hasRelatedWork W2026459329 @default.
• W2076636650 hasRelatedWork W2046739381 @default.
• W2076636650 hasRelatedWork W2073037709 @default.
• W2076636650 hasRelatedWork W2079830704 @default.
• W2076636650 hasRelatedWork W2082842399 @default.
• W2076636650 hasRelatedWork W2347388628 @default.
• W2076636650 hasRelatedWork W2361053869 @default.
• W2076636650 hasRelatedWork W2800280878 @default.
• W2076636650 hasRelatedWork W889929647 @default.
• W2076636650 hasRelatedWork W2087222142 @default.
• W2076636650 hasVolume "182" @default.
• W2076636650 isParatext "false" @default.
• W2076636650 isRetracted "false" @default.
• W2076636650 magId "2076636650" @default.

• next