FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2960330398> ?p ?o ?g. }

• W2960330398 endingPage "61" @default.
• W2960330398 startingPage "44" @default.
• W2960330398 abstract "The widespread late Carboniferous calc-alkaline and shoshonitic magmatic rocks in the Awulale mountain provide crucial constraints on the tectonic evolution of the western Tianshan. Here, we perform detailed petrological investigations as well as zircon U-Pb chronological, whole-rock geochemical and Sr-Nd isotopic analyses on these magmatic rocks from two geological sections along the Duku road. Magmatic rocks in the section I with zircon SHRIMP U-Pb ages of 306.8 Ma and 306.4 Ma are composed of medium-K calc-alkaline to shoshonitic basalt, trachy-andesite and trachyte, while those in the section II consist of shoshonitic trachy-andesite, trachyte with a U-Pb age of 308.1 Ma, and monzonite with a U-Pb age of 309.6 Ma. All these magmatic rocks are characterized by strong enrichments in large iron lithophile elements with depletions of Nb, Ta and Ti, indicating the origination from subduction-modified lithospheric mantle. The εNd(t) values of the rock samples collected from the section I (2.80–5.45) and section II (3.34–5.37) are generally higher than those of the Devonian to early Carboniferous arc-type magmatic rocks in the Yili-central Tianshan, suggesting that depleted asthenosphere might also be involved in their generation. Based on these geochemical data and petrological observations, we suggest that the early-stage (308.1–309.6 Ma) shoshonitic monzonite, trachy-andesite and trachyte in the section II were generated by mixing between mafic magmas and trachytic melts, while the late-stage (306.4–306.8 Ma) medium-K calc-alkaline to shoshonitic basalt, trachy-andesite and trachyte in the section I were produced by partial melting of depleted asthenospheric and metasomatized lithospheric mantle, followed by the processes of fractional crystallization and crustal contamination. Taking into account the available regional geological data, the subduction of south Tianshan ocean was probably ceased at ∼310 Ma, and these calc-alkaline and shoshonitic magmatic rocks in the Awulale mountain formed in a post-collisional setting subsequent to slab break-off." @default.
• W2960330398 created "2019-07-23" @default.
• W2960330398 creator A5038398029 @default.
• W2960330398 creator A5077205000 @default.
• W2960330398 date "2019-12-01" @default.
• W2960330398 modified "2023-10-05" @default.
• W2960330398 title "Petrogenesis and tectonic implications of the late Carboniferous calc-alkaline and shoshonitic magmatic rocks in the Awulale mountain, western Tianshan" @default.
• W2960330398 cites W1863083957 @default.
• W2960330398 cites W1975325913 @default.
• W2960330398 cites W1975787055 @default.
• W2960330398 cites W1976304054 @default.
• W2960330398 cites W1977036594 @default.
• W2960330398 cites W1979634734 @default.
• W2960330398 cites W1983624300 @default.
• W2960330398 cites W1985567940 @default.
• W2960330398 cites W1986717974 @default.
• W2960330398 cites W1995350298 @default.
• W2960330398 cites W1998248723 @default.
• W2960330398 cites W2002822830 @default.
• W2960330398 cites W2014992926 @default.
• W2960330398 cites W2018398267 @default.
• W2960330398 cites W2019531829 @default.
• W2960330398 cites W2024263269 @default.
• W2960330398 cites W2036813892 @default.
• W2960330398 cites W2040565276 @default.
• W2960330398 cites W2048770061 @default.
• W2960330398 cites W2049626686 @default.
• W2960330398 cites W2064241548 @default.
• W2960330398 cites W2064723292 @default.
• W2960330398 cites W2069358088 @default.
• W2960330398 cites W2069402922 @default.
• W2960330398 cites W2072600594 @default.
• W2960330398 cites W2072608003 @default.
• W2960330398 cites W2077011553 @default.
• W2960330398 cites W2077285302 @default.
• W2960330398 cites W2078009831 @default.
• W2960330398 cites W2081213487 @default.
• W2960330398 cites W2081673195 @default.
• W2960330398 cites W2082867332 @default.
• W2960330398 cites W2083815617 @default.
• W2960330398 cites W2088897934 @default.
• W2960330398 cites W2094767644 @default.
• W2960330398 cites W2124276467 @default.
• W2960330398 cites W2128834298 @default.
• W2960330398 cites W2137588825 @default.
• W2960330398 cites W2138522501 @default.
• W2960330398 cites W2140149446 @default.
• W2960330398 cites W2143093330 @default.
• W2960330398 cites W2152621320 @default.
• W2960330398 cites W2157099954 @default.
• W2960330398 cites W2159297868 @default.
• W2960330398 cites W2216920053 @default.
• W2960330398 cites W2227501935 @default.
• W2960330398 cites W2312828419 @default.
• W2960330398 cites W2415803713 @default.
• W2960330398 cites W2433653237 @default.
• W2960330398 cites W2514574042 @default.
• W2960330398 cites W2549493607 @default.
• W2960330398 cites W2551782820 @default.
• W2960330398 cites W2574770532 @default.
• W2960330398 cites W2583448077 @default.
• W2960330398 cites W2591752739 @default.
• W2960330398 cites W2596849444 @default.
• W2960330398 cites W2600915275 @default.
• W2960330398 cites W2601690688 @default.
• W2960330398 cites W2607933998 @default.
• W2960330398 cites W2616011372 @default.
• W2960330398 cites W2625327173 @default.
• W2960330398 cites W2735201426 @default.
• W2960330398 cites W2757538466 @default.
• W2960330398 cites W2760881469 @default.
• W2960330398 cites W2767370723 @default.
• W2960330398 cites W2770388368 @default.
• W2960330398 cites W2772792706 @default.
• W2960330398 cites W2775810706 @default.
• W2960330398 cites W2776626375 @default.
• W2960330398 cites W2799949189 @default.
• W2960330398 cites W2803213217 @default.
• W2960330398 cites W2804060750 @default.
• W2960330398 cites W2885412976 @default.
• W2960330398 cites W2892656178 @default.
• W2960330398 cites W2893579742 @default.
• W2960330398 cites W2907110425 @default.
• W2960330398 cites W3143049761 @default.
• W2960330398 cites W4372123854 @default.
• W2960330398 cites W799622644 @default.
• W2960330398 doi "https://doi.org/10.1016/j.gr.2019.05.009" @default.
• W2960330398 hasPublicationYear "2019" @default.
• W2960330398 type Work @default.
• W2960330398 sameAs 2960330398 @default.
• W2960330398 citedByCount "18" @default.
• W2960330398 countsByYear W29603303982019 @default.
• W2960330398 countsByYear W29603303982020 @default.
• W2960330398 countsByYear W29603303982021 @default.
• W2960330398 countsByYear W29603303982022 @default.
• W2960330398 countsByYear W29603303982023 @default.
• W2960330398 crossrefType "journal-article" @default.
• W2960330398 hasAuthorship W2960330398A5038398029 @default.

• next