FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2077602012> ?p ?o ?g. }

• W2077602012 endingPage "71" @default.
• W2077602012 startingPage "56" @default.
• W2077602012 abstract "Abstract The Oligocene–Miocene Zivah Formation is characterised by alternation of sandstone, conglomerate, and shale that were deposited in a fluvial dominated delta on the shelf of Eastern Paratethys. Petrographically, the sandstones mostly include volcanic rock fragment, plagioclase and minor amounts of K feldspar, quartz, pyroxene, opaque minerals and biotite. Heavy mineral analysis and geochemical analysis of detrital clinopyroxene and apatite have been used to determine the provenance and tectonic setting of the Zivah Formation sandstones, in three outcrop sections from the Moghan region in NW Iran. The heavy mineral assemblage of the Zivah Formation sandstones is dominated by clinopyroxene and apatite with minor amounts of amphibole, zircon, garnet and epidote. The abundance of a mafic heavy-mineral suite such as clinopyroxene relative to metamorphic and felsic heavy mineral suites such as epidote, garnet and zircon indicates that deposition of Zivah Formation is more likely to have occurred at a convergent plate boundary, and sourced by a volcanic arc. The geochemical composition of detrital clinopyroxene grains from the Zivah Formation indicates that these detrital grains probably crystallized from calk-alkaline magmas. They also show an orogenic tectonic setting at the time of deposition of the Zivah Formation. Compositions of detrital apatites of the Zivah Formation are also consistent with the widespread distribution of mafic/intermediate volcanic rocks of both alkaline and calc-alkaline composition. All of these data as well as the composition of volcanic rocks of the southern parts of the Moghan Basin is consistent with the derivation of these sediments from areas with calc-alkaline volcanic rocks like Talysh and Arasbaran (Qharadagh)–Lesser Caucasus." @default.
• W2077602012 created "2016-06-24" @default.
• W2077602012 creator A5009394991 @default.
• W2077602012 creator A5021218644 @default.
• W2077602012 creator A5031858639 @default.
• W2077602012 creator A5035005219 @default.
• W2077602012 creator A5059732793 @default.
• W2077602012 creator A5061491240 @default.
• W2077602012 date "2014-01-01" @default.
• W2077602012 modified "2023-09-23" @default.
• W2077602012 title "Provenance of the Oligocene–Miocene Zivah Formation, NW Iran, assessed using heavy mineral assemblage and detrital clinopyroxene and detrital apatite analyses" @default.
• W2077602012 cites W134798769 @default.
• W2077602012 cites W1505548605 @default.
• W2077602012 cites W1505838194 @default.
• W2077602012 cites W1534180280 @default.
• W2077602012 cites W1967831326 @default.
• W2077602012 cites W1971765041 @default.
• W2077602012 cites W1972402506 @default.
• W2077602012 cites W1976630555 @default.
• W2077602012 cites W1981054075 @default.
• W2077602012 cites W1981536455 @default.
• W2077602012 cites W1991220051 @default.
• W2077602012 cites W1994025467 @default.
• W2077602012 cites W2003815807 @default.
• W2077602012 cites W2008732209 @default.
• W2077602012 cites W2008907905 @default.
• W2077602012 cites W2009975688 @default.
• W2077602012 cites W2013056732 @default.
• W2077602012 cites W2025156170 @default.
• W2077602012 cites W2025294455 @default.
• W2077602012 cites W2033551932 @default.
• W2077602012 cites W2036580797 @default.
• W2077602012 cites W2040326637 @default.
• W2077602012 cites W2043339008 @default.
• W2077602012 cites W2044880652 @default.
• W2077602012 cites W2059797972 @default.
• W2077602012 cites W2059920600 @default.
• W2077602012 cites W2069499712 @default.
• W2077602012 cites W2073440017 @default.
• W2077602012 cites W2074141659 @default.
• W2077602012 cites W2086343310 @default.
• W2077602012 cites W2090457820 @default.
• W2077602012 cites W2110837005 @default.
• W2077602012 cites W2141890535 @default.
• W2077602012 cites W2142229802 @default.
• W2077602012 cites W2143603242 @default.
• W2077602012 cites W2152371718 @default.
• W2077602012 cites W2162557247 @default.
• W2077602012 cites W2169631125 @default.
• W2077602012 cites W2214699775 @default.
• W2077602012 cites W4211032377 @default.
• W2077602012 cites W4244513166 @default.
• W2077602012 doi "https://doi.org/10.1016/j.jafrearsci.2013.10.005" @default.
• W2077602012 hasPublicationYear "2014" @default.
• W2077602012 type Work @default.
• W2077602012 sameAs 2077602012 @default.
• W2077602012 citedByCount "20" @default.
• W2077602012 countsByYear W20776020122014 @default.
• W2077602012 countsByYear W20776020122015 @default.
• W2077602012 countsByYear W20776020122016 @default.
• W2077602012 countsByYear W20776020122018 @default.
• W2077602012 countsByYear W20776020122019 @default.
• W2077602012 countsByYear W20776020122020 @default.
• W2077602012 countsByYear W20776020122021 @default.
• W2077602012 countsByYear W20776020122022 @default.
• W2077602012 countsByYear W20776020122023 @default.
• W2077602012 crossrefType "journal-article" @default.
• W2077602012 hasAuthorship W2077602012A5009394991 @default.
• W2077602012 hasAuthorship W2077602012A5021218644 @default.
• W2077602012 hasAuthorship W2077602012A5031858639 @default.
• W2077602012 hasAuthorship W2077602012A5035005219 @default.
• W2077602012 hasAuthorship W2077602012A5059732793 @default.
• W2077602012 hasAuthorship W2077602012A5061491240 @default.
• W2077602012 hasConcept C127313418 @default.
• W2077602012 hasConcept C151730666 @default.
• W2077602012 hasConcept C17409809 @default.
• W2077602012 hasConcept C191897082 @default.
• W2077602012 hasConcept C192562407 @default.
• W2077602012 hasConcept C2776432453 @default.
• W2077602012 hasConcept C2777746296 @default.
• W2077602012 hasConcept C2777798969 @default.
• W2077602012 hasConcept C2780049196 @default.
• W2077602012 hasConcept C2781394513 @default.
• W2077602012 hasConceptScore W2077602012C127313418 @default.
• W2077602012 hasConceptScore W2077602012C151730666 @default.
• W2077602012 hasConceptScore W2077602012C17409809 @default.
• W2077602012 hasConceptScore W2077602012C191897082 @default.
• W2077602012 hasConceptScore W2077602012C192562407 @default.
• W2077602012 hasConceptScore W2077602012C2776432453 @default.
• W2077602012 hasConceptScore W2077602012C2777746296 @default.
• W2077602012 hasConceptScore W2077602012C2777798969 @default.
• W2077602012 hasConceptScore W2077602012C2780049196 @default.
• W2077602012 hasConceptScore W2077602012C2781394513 @default.
• W2077602012 hasLocation W20776020121 @default.
• W2077602012 hasOpenAccess W2077602012 @default.
• W2077602012 hasPrimaryLocation W20776020121 @default.
• W2077602012 hasRelatedWork W1982747566 @default.
• W2077602012 hasRelatedWork W2005522291 @default.

• next