FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2055362357> ?p ?o ?g. }

• W2055362357 endingPage "493" @default.
• W2055362357 startingPage "481" @default.
• W2055362357 abstract "The Hangay–Hentey belt is situated in the central Northern Mongolia, and forms part of the Central Asian Orogenic Belt (CAOB). It is internally subdivided into seven terranes, the largest of which are the neighbouring Ulaanbaatar and Tsetserleg terranes. These coeval terranes are mainly composed of Silurian–Devonian accretionary complexes and Carboniferous turbidites. Proposals for their depositional setting range from passive margin through to island arc. A suite of 19 Ulaanbaatar terrane sandstones and mudrocks (Gorkhi and Altanovoo Formations) were collected with the aim of constraining their provenance, source weathering, and depositional setting based on whole-rock major and trace element data, and for comparison with the neighbouring Tsetserleg terrane. New REE analyses were also made of 35 samples from the Ulaanbaatar and Tsetserleg terranes. Geochemically the Ulaanbaatar sandstones are classed as wackes, and most of the mudstones as shales. Geochemical parameters suggest an immature source, similar to that of the Tsetserleg terrane. Geochemical contrasts between sandstones and mudrocks in the Ulaanbaatar sediments are small, and trends on element – Al2O3 variation diagrams are weak. Comparison with average upper continental crust (UCC), major element discriminant scores, and immobile element ratios (Th/Sc, Zr/Sc, Ce/Sc, Ti/Zr) indicate a uniform average source composition between dacite and rhyolite. Maximum Chemical Index of Alteration value in the Ulaanbaatar terrane is ∼65 after correction for K-metasomatism, indicating minimal weathering in a tectonically active source, similar to that of the Tsetserleg terrane. REE data in both terranes show moderate LREE enrichment and flat HREE segments, with negative Eu anomalies somewhat less than those in UCC and PAAS. Chondrite-normalized patterns are very similar to that for average Paleozoic felsic volcanic rock, supporting the relatively felsic source indicated by immobile trace element ratios. Tectonic setting discriminants (K2O/Na2O–SiO2/Al2O3, La–Th–Sc, Th–Sc–Zr) indicate an evolved continental island arc (CIA; A2) environment for both terranes, similar to several other CAOB suites of similar age. This common arc source was situated within the Mongol-Okhotsk Ocean during Silurian–Lower Carboniferous time. The present-day Aleutian arc is a possible modern analogue of the depositional setting." @default.
• W2055362357 created "2016-06-24" @default.
• W2055362357 creator A5016612547 @default.
• W2055362357 creator A5067417755 @default.
• W2055362357 date "2013-12-01" @default.
• W2055362357 modified "2023-09-28" @default.
• W2055362357 title "Geochemistry of Silurian–Carboniferous sedimentary rocks of the Ulaanbaatar terrane, Hangay–Hentey belt, central Mongolia: Provenance, paleoweathering, tectonic setting, and relationship with the neighbouring Tsetserleg terrane" @default.
• W2055362357 cites W1540983220 @default.
• W2055362357 cites W1965701586 @default.
• W2055362357 cites W1967346487 @default.
• W2055362357 cites W1975042776 @default.
• W2055362357 cites W1983181201 @default.
• W2055362357 cites W1988873014 @default.
• W2055362357 cites W1996553891 @default.
• W2055362357 cites W1997705537 @default.
• W2055362357 cites W1998670404 @default.
• W2055362357 cites W2008127132 @default.
• W2055362357 cites W2014935809 @default.
• W2055362357 cites W2015876559 @default.
• W2055362357 cites W2016223358 @default.
• W2055362357 cites W2016848487 @default.
• W2055362357 cites W2019949618 @default.
• W2055362357 cites W2029401070 @default.
• W2055362357 cites W2034223887 @default.
• W2055362357 cites W2040236851 @default.
• W2055362357 cites W2041276447 @default.
• W2055362357 cites W2043844425 @default.
• W2055362357 cites W2050716036 @default.
• W2055362357 cites W2057228997 @default.
• W2055362357 cites W2065999153 @default.
• W2055362357 cites W2075349472 @default.
• W2055362357 cites W2076610107 @default.
• W2055362357 cites W2081554454 @default.
• W2055362357 cites W2089096123 @default.
• W2055362357 cites W2094117407 @default.
• W2055362357 cites W2118657171 @default.
• W2055362357 cites W2124460270 @default.
• W2055362357 cites W2170868101 @default.
• W2055362357 cites W2247098479 @default.
• W2055362357 cites W2331272198 @default.
• W2055362357 cites W284642688 @default.
• W2055362357 cites W2972310400 @default.
• W2055362357 doi "https://doi.org/10.1016/j.chemer.2013.03.003" @default.
• W2055362357 hasPublicationYear "2013" @default.
• W2055362357 type Work @default.
• W2055362357 sameAs 2055362357 @default.
• W2055362357 citedByCount "22" @default.
• W2055362357 countsByYear W20553623572014 @default.
• W2055362357 countsByYear W20553623572015 @default.
• W2055362357 countsByYear W20553623572016 @default.
• W2055362357 countsByYear W20553623572017 @default.
• W2055362357 countsByYear W20553623572018 @default.
• W2055362357 countsByYear W20553623572019 @default.
• W2055362357 countsByYear W20553623572020 @default.
• W2055362357 countsByYear W20553623572021 @default.
• W2055362357 countsByYear W20553623572022 @default.
• W2055362357 countsByYear W20553623572023 @default.
• W2055362357 crossrefType "journal-article" @default.
• W2055362357 hasAuthorship W2055362357A5016612547 @default.
• W2055362357 hasAuthorship W2055362357A5067417755 @default.
• W2055362357 hasConcept C109007969 @default.
• W2055362357 hasConcept C126753816 @default.
• W2055362357 hasConcept C127313418 @default.
• W2055362357 hasConcept C141646446 @default.
• W2055362357 hasConcept C150999391 @default.
• W2055362357 hasConcept C151730666 @default.
• W2055362357 hasConcept C167284885 @default.
• W2055362357 hasConcept C17409809 @default.
• W2055362357 hasConcept C193429443 @default.
• W2055362357 hasConcept C2776698055 @default.
• W2055362357 hasConcept C2780049196 @default.
• W2055362357 hasConcept C5900021 @default.
• W2055362357 hasConcept C77928131 @default.
• W2055362357 hasConceptScore W2055362357C109007969 @default.
• W2055362357 hasConceptScore W2055362357C126753816 @default.
• W2055362357 hasConceptScore W2055362357C127313418 @default.
• W2055362357 hasConceptScore W2055362357C141646446 @default.
• W2055362357 hasConceptScore W2055362357C150999391 @default.
• W2055362357 hasConceptScore W2055362357C151730666 @default.
• W2055362357 hasConceptScore W2055362357C167284885 @default.
• W2055362357 hasConceptScore W2055362357C17409809 @default.
• W2055362357 hasConceptScore W2055362357C193429443 @default.
• W2055362357 hasConceptScore W2055362357C2776698055 @default.
• W2055362357 hasConceptScore W2055362357C2780049196 @default.
• W2055362357 hasConceptScore W2055362357C5900021 @default.
• W2055362357 hasConceptScore W2055362357C77928131 @default.
• W2055362357 hasFunder F4320326473 @default.
• W2055362357 hasIssue "4" @default.
• W2055362357 hasLocation W20553623571 @default.
• W2055362357 hasOpenAccess W2055362357 @default.
• W2055362357 hasPrimaryLocation W20553623571 @default.
• W2055362357 hasRelatedWork W2042444662 @default.
• W2055362357 hasRelatedWork W2049581925 @default.
• W2055362357 hasRelatedWork W2094174094 @default.
• W2055362357 hasRelatedWork W2349903556 @default.
• W2055362357 hasRelatedWork W2886178728 @default.
• W2055362357 hasRelatedWork W2911405760 @default.
• W2055362357 hasRelatedWork W3011836163 @default.

• next