FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2016151030> ?p ?o ?g. }

• W2016151030 endingPage "147" @default.
• W2016151030 startingPage "131" @default.
• W2016151030 abstract "Late Paleozoic post-collisional granitoids are widespread in West Junggar, as well as northern Xinjiang. As a representative of those intrusions, the Jietebutiao granite occurs in the southwestern margin of the West Junggar (northwest China), and is mainly composed of mid-coarse-grained monzogranite and syenogranite. In the present study, we report the results of high-precision zircon laser-ablation–inductively-coupled plasma mass–spectrometry U–Pb dating on the Jietebutiao granite for the first time, and yield weighted mean 206Pb/238U ages of 287 ± 9 Ma and 278 ± 3 Ma for monzogranite and syenogranite, respectively. The Jietebutiao granite has a pronounced A-type affinity; it is metaluminons to slightly peraluminous; has a high-K calc-alkaline composition; high concentrations of Na2O + K2O, varying from 6.8 to 8.5 wt%; high FeOt/MgO; 10 000Ga/Al ratios, a low CaO, MgO, and TiO2 content; enriched in some large ion lithophile elements (LILE, such as Rb and Th) and high field strength elements (HFSE, such as Zr, Hf, and Y); and depleted in Sr, Ba, and Ti. In addition, the granite has a relatively high rare earth element (REE) content (except for Eu), with significant negative Eu anomalies (Eu/Eu*= 0.01–0.72), and showing slight tetrad REE patterns and non-charge and radius controlled (CHARAC) trace element behavior. Petrographic, geochemical, and geochronological data suggest that the parental magma of Jietebutiao intrusions are of mixed origin, and are most probably formed by the interaction between the lower crust- and mantle-derived magmas in the Early Permian post-collisional tectonic setting. The basaltic magmas underplated and interacted with the lower crust that was dominated by deeply buried arc (and back-arc basin) series and the oceanic crust formed in the Paleozoic, and then triggered the partial melting of the juvenile lower crust, producing voluminous granitic melts and forming the Jietebutiao A2-type monzogranites, with the lithospheric mantle progressively thinning and rifting to form A-type granites, such as syenogranites, in the Jietebutiao pluton. This further proves the important contribution of Late Paleozoic granitic magmatism in terms of vertical crustal growth in northern Xinjiang." @default.
• W2016151030 created "2016-06-24" @default.
• W2016151030 creator A5020329063 @default.
• W2016151030 creator A5032049970 @default.
• W2016151030 creator A5044706230 @default.
• W2016151030 creator A5062125985 @default.
• W2016151030 creator A5082947244 @default.
• W2016151030 creator A5089650343 @default.
• W2016151030 date "2013-02-01" @default.
• W2016151030 modified "2023-09-27" @default.
• W2016151030 title "Geochronological and Geochemical Constrains on Petrogenesis of the Jietebutiao A-type Granite in West Junggar, Xinjiang" @default.
• W2016151030 cites W1489853072 @default.
• W2016151030 cites W1514994218 @default.
• W2016151030 cites W1533138910 @default.
• W2016151030 cites W1555507089 @default.
• W2016151030 cites W183765136 @default.
• W2016151030 cites W1965835831 @default.
• W2016151030 cites W1967827341 @default.
• W2016151030 cites W1968450376 @default.
• W2016151030 cites W1971685925 @default.
• W2016151030 cites W1974499954 @default.
• W2016151030 cites W1977305335 @default.
• W2016151030 cites W1977650828 @default.
• W2016151030 cites W1978676610 @default.
• W2016151030 cites W1979473511 @default.
• W2016151030 cites W1979694545 @default.
• W2016151030 cites W1979918251 @default.
• W2016151030 cites W1983058322 @default.
• W2016151030 cites W1984923148 @default.
• W2016151030 cites W1988317790 @default.
• W2016151030 cites W1990101516 @default.
• W2016151030 cites W1990169677 @default.
• W2016151030 cites W1992832689 @default.
• W2016151030 cites W1994804633 @default.
• W2016151030 cites W1997438303 @default.
• W2016151030 cites W1999708461 @default.
• W2016151030 cites W2001552374 @default.
• W2016151030 cites W2002469616 @default.
• W2016151030 cites W2003323528 @default.
• W2016151030 cites W2006510222 @default.
• W2016151030 cites W2008225735 @default.
• W2016151030 cites W2008442425 @default.
• W2016151030 cites W2012452556 @default.
• W2016151030 cites W2014165584 @default.
• W2016151030 cites W2014722475 @default.
• W2016151030 cites W2016025369 @default.
• W2016151030 cites W2019034794 @default.
• W2016151030 cites W2022859730 @default.
• W2016151030 cites W2023280097 @default.
• W2016151030 cites W2024920534 @default.
• W2016151030 cites W2026771566 @default.
• W2016151030 cites W2032296046 @default.
• W2016151030 cites W2033683037 @default.
• W2016151030 cites W2034732315 @default.
• W2016151030 cites W2036642627 @default.
• W2016151030 cites W2039100744 @default.
• W2016151030 cites W2039485407 @default.
• W2016151030 cites W2041735703 @default.
• W2016151030 cites W2042803182 @default.
• W2016151030 cites W2044934678 @default.
• W2016151030 cites W2047180528 @default.
• W2016151030 cites W2058019619 @default.
• W2016151030 cites W2059250966 @default.
• W2016151030 cites W2062920764 @default.
• W2016151030 cites W2063964861 @default.
• W2016151030 cites W2065065857 @default.
• W2016151030 cites W2071103381 @default.
• W2016151030 cites W2074233105 @default.
• W2016151030 cites W2075964210 @default.
• W2016151030 cites W2078105240 @default.
• W2016151030 cites W2078374032 @default.
• W2016151030 cites W2079767098 @default.
• W2016151030 cites W2081309949 @default.
• W2016151030 cites W2085981782 @default.
• W2016151030 cites W2089096123 @default.
• W2016151030 cites W2092217821 @default.
• W2016151030 cites W2093260086 @default.
• W2016151030 cites W2093672791 @default.
• W2016151030 cites W2094985587 @default.
• W2016151030 cites W2103463307 @default.
• W2016151030 cites W2108971421 @default.
• W2016151030 cites W2112109341 @default.
• W2016151030 cites W2120370873 @default.
• W2016151030 cites W2124044757 @default.
• W2016151030 cites W2124276467 @default.
• W2016151030 cites W2125160417 @default.
• W2016151030 cites W2125585433 @default.
• W2016151030 cites W2128624170 @default.
• W2016151030 cites W2138037224 @default.
• W2016151030 cites W2138522501 @default.
• W2016151030 cites W2139788788 @default.
• W2016151030 cites W2144081161 @default.
• W2016151030 cites W2144701379 @default.
• W2016151030 cites W2152222036 @default.
• W2016151030 cites W2153500334 @default.
• W2016151030 cites W2162997816 @default.
• W2016151030 cites W2164468447 @default.
• W2016151030 cites W2167145749 @default.

• next