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• W4321374658 endingPage "290" @default.
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• W4321374658 abstract "The rhyolites which are widely exposed to the northern margin of the East Kunlun orogenic belt were chosen as a research object to discern the post-orogenic tectonic evolution of the East Kunlun orogenic belt and reconstruct the post-collision orogenic processes of the Buqingshan- A’nyemaqen Ocean. We researched zircon U-Pb ages and geochemistry characteristics of the Late Triassic rhyolites in the eastern segment of the East Kunlun Orogenic Belt in the northern Tibetan Plateau. Zircon U-Pb dating yields coeval ages of 200.4 ± 1.4 Ma and 202.8 ± 1.2 Ma for the Keri rhyolites of the East Kunlun Orogenic Belt, indicating that the volcanic rocks were formed in the Late Triassic Rhaetian–Early Jurassic Hettangian. The Keri rhyolite is a product of the late magmatism of the Elashan Formation volcanic rocks. The rhyolites include rhyolitic brecciated tuff lavas and rhyolitic tuff lavas. The rhyolites are peraluminous and are high-K calc-alkaline, with high contents of SiO2, K2O, TFe2O3, and low P2O5 contents. The A/CNK ratios range from 0.97 to 1.09, indicating that the rhyolites are metaluminous to weakly peraluminous. The chondrite-normalized rare earth element (REE) distribution shows a significant negative Eu anomaly and low total REE concentrations. All samples are depleted in high field strength elements (HFSEs, e.g., Eu, Sr, Ti, and P), heavy rare earth elements (HREEs), and enriched in large ion lithophile elements (LILEs, e.g., Rb, Zr, Nd, Th, and U) and light rare earth elements (LREEs). The Keri rhyolite has the characteristics of A1-type magmatic rock, formed in an anorogenic environment after the closure of the Paleo-Tethys Ocean, and was the product of late magmatism in the Elashan Formation volcanic rocks." @default.
• W4321374658 created "2023-02-21" @default.
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• W4321374658 date "2023-02-18" @default.
• W4321374658 modified "2023-09-25" @default.
• W4321374658 title "Petrogenesis and Geochronology of A1-Type Rhyolites in the Late Late Triassic of the East Kunlun Orogenic Belt: Constraints on the End of the Paleo-Tethys Orogenic Event" @default.
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• W4321374658 cites W1974499954 @default.
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• W4321374658 cites W1986675831 @default.
• W4321374658 cites W1986949096 @default.
• W4321374658 cites W1995884346 @default.
• W4321374658 cites W1998160016 @default.
• W4321374658 cites W2000661276 @default.
• W4321374658 cites W2007251492 @default.
• W4321374658 cites W2008335913 @default.
• W4321374658 cites W2012715340 @default.
• W4321374658 cites W2017531788 @default.
• W4321374658 cites W2019034794 @default.
• W4321374658 cites W2022859730 @default.
• W4321374658 cites W2023388876 @default.
• W4321374658 cites W2026245988 @default.
• W4321374658 cites W2026287564 @default.
• W4321374658 cites W2027205257 @default.
• W4321374658 cites W2036413971 @default.
• W4321374658 cites W2036884486 @default.
• W4321374658 cites W2040029696 @default.
• W4321374658 cites W2041560786 @default.
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• W4321374658 cites W2046961523 @default.
• W4321374658 cites W2055995241 @default.
• W4321374658 cites W2059250966 @default.
• W4321374658 cites W2074233105 @default.
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• W4321374658 cites W2095803901 @default.
• W4321374658 cites W2101782242 @default.
• W4321374658 cites W2108971421 @default.
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• W4321374658 cites W2138482043 @default.
• W4321374658 cites W2138522501 @default.
• W4321374658 cites W2144081161 @default.
• W4321374658 cites W2145173997 @default.
• W4321374658 cites W2159585010 @default.
• W4321374658 cites W2162763302 @default.
• W4321374658 cites W2167856052 @default.
• W4321374658 cites W2168769600 @default.
• W4321374658 cites W2170189319 @default.
• W4321374658 cites W2170736074 @default.
• W4321374658 cites W2171405411 @default.
• W4321374658 cites W2403988321 @default.
• W4321374658 cites W2557512738 @default.
• W4321374658 cites W2594721306 @default.
• W4321374658 cites W2620353602 @default.
• W4321374658 cites W2773960655 @default.
• W4321374658 cites W2801110655 @default.
• W4321374658 cites W2946301465 @default.
• W4321374658 cites W2947478775 @default.
• W4321374658 cites W2948551475 @default.
• W4321374658 cites W2973166275 @default.
• W4321374658 cites W2990292477 @default.
• W4321374658 cites W299078247 @default.
• W4321374658 cites W2994947805 @default.
• W4321374658 cites W2995482781 @default.
• W4321374658 cites W3008733407 @default.
• W4321374658 cites W3014492166 @default.
• W4321374658 cites W3111671544 @default.
• W4321374658 cites W3127877316 @default.
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• W4321374658 cites W4206679919 @default.
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• W4321374658 cites W4309039452 @default.
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• W4321374658 doi "https://doi.org/10.3390/min13020290" @default.
• W4321374658 hasPublicationYear "2023" @default.
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