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• W2024444204 endingPage "113" @default.
• W2024444204 startingPage "100" @default.
• W2024444204 abstract "Modal, chemical and U–Pb zircon data from Permian sandstones in the central and southern Da Xing'an Mountains (eastern Inner Mongolia, China) constrain, for the first time, plate collision processes between the northern margin of the North China craton and the composite Erguna–Xing'an–Songliao block. The study area is located between the Ondor Sum-Xar Moron and Hegenshan suture zones of the eastern segment of the Central Asian Orogenic Belt. Modal and geochemical analyses of Permian sandstones suggest derivation from dissected continental arc and recycled orogenic sources. LA-ICP-MS U–Pb detrital zircon data from sandstones indicate Early Permian to earliest Triassic maximum depositional ages (278 ± 4 Ma to 249 ± 3 Ma). These data also show two uniform age groups of 270–280 Ma and 310–320 Ma, and we interpret their source to be mainly the Sonidzuoqi–Xilinhot–southern Xi Ujimqin magmatic arc in the north (the southern margin of the Xing'an–Erguna block). The sample from the Upper Permian to lowermost Triassic Linxi Formation in the Linxi area also contains zircons with age groups of ~ 1800 Ma and ~ 2500 Ma, consistent with derivation from the northern margin of the North China craton, which lies to the south. Therefore, the collision between the North China craton and the Xing'an–Erguna block began during the deposition of the Linxi Formation, and the final closure of the intervening oceanic basin occurred during ca. Late Permian–earliest Triassic times, forming the Ondor Sum-Xar Moron suture zone." @default.
• W2024444204 created "2016-06-24" @default.
• W2024444204 creator A5005125989 @default.
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• W2024444204 creator A5091882350 @default.
• W2024444204 date "2012-12-01" @default.
• W2024444204 modified "2023-10-12" @default.
• W2024444204 title "Provenance analysis of Permian sandstones in the central and southern Da Xing'an Mountains, China: Constraints on the evolution of the eastern segment of the Central Asian Orogenic Belt" @default.
• W2024444204 cites W1504892392 @default.
• W2024444204 cites W1615451124 @default.
• W2024444204 cites W183765136 @default.
• W2024444204 cites W1967827341 @default.
• W2024444204 cites W1969371403 @default.
• W2024444204 cites W1970439132 @default.
• W2024444204 cites W1974413429 @default.
• W2024444204 cites W1978257403 @default.
• W2024444204 cites W1978904154 @default.
• W2024444204 cites W1982291435 @default.
• W2024444204 cites W1983072117 @default.
• W2024444204 cites W1986983284 @default.
• W2024444204 cites W1988317790 @default.
• W2024444204 cites W1988632867 @default.
• W2024444204 cites W1988828197 @default.
• W2024444204 cites W1989194022 @default.
• W2024444204 cites W1990701109 @default.
• W2024444204 cites W1991323502 @default.
• W2024444204 cites W1992721858 @default.
• W2024444204 cites W1995897602 @default.
• W2024444204 cites W1999621813 @default.
• W2024444204 cites W2003323528 @default.
• W2024444204 cites W2003348019 @default.
• W2024444204 cites W2015620905 @default.
• W2024444204 cites W2015876559 @default.
• W2024444204 cites W2017587656 @default.
• W2024444204 cites W2018790242 @default.
• W2024444204 cites W2019259962 @default.
• W2024444204 cites W2019949618 @default.
• W2024444204 cites W2025402991 @default.
• W2024444204 cites W2026287564 @default.
• W2024444204 cites W2029506771 @default.
• W2024444204 cites W2030056256 @default.
• W2024444204 cites W2032353260 @default.
• W2024444204 cites W2032369168 @default.
• W2024444204 cites W2034223887 @default.
• W2024444204 cites W2039511246 @default.
• W2024444204 cites W2043003723 @default.
• W2024444204 cites W2044349582 @default.
• W2024444204 cites W2045389864 @default.
• W2024444204 cites W2047764283 @default.
• W2024444204 cites W2054366973 @default.
• W2024444204 cites W2057709663 @default.
• W2024444204 cites W2060461428 @default.
• W2024444204 cites W2065092571 @default.
• W2024444204 cites W2068038089 @default.
• W2024444204 cites W2068365898 @default.
• W2024444204 cites W2070751239 @default.
• W2024444204 cites W2071432070 @default.
• W2024444204 cites W2072664369 @default.
• W2024444204 cites W2075694434 @default.
• W2024444204 cites W2078251097 @default.
• W2024444204 cites W2085431448 @default.
• W2024444204 cites W2089096123 @default.
• W2024444204 cites W2089426009 @default.
• W2024444204 cites W2091071952 @default.
• W2024444204 cites W2091749701 @default.
• W2024444204 cites W2093672791 @default.
• W2024444204 cites W2103463307 @default.
• W2024444204 cites W2106161981 @default.
• W2024444204 cites W2110416396 @default.
• W2024444204 cites W2110531414 @default.
• W2024444204 cites W2118364502 @default.
• W2024444204 cites W2119991869 @default.
• W2024444204 cites W2122059422 @default.
• W2024444204 cites W2124460270 @default.
• W2024444204 cites W2125160417 @default.
• W2024444204 cites W2126127241 @default.
• W2024444204 cites W2130869872 @default.
• W2024444204 cites W2134490602 @default.
• W2024444204 cites W2144629160 @default.
• W2024444204 cites W2146820948 @default.
• W2024444204 cites W2150092572 @default.
• W2024444204 cites W2162457106 @default.
• W2024444204 cites W2165712457 @default.
• W2024444204 cites W2169016685 @default.
• W2024444204 cites W2170684487 @default.
• W2024444204 cites W2170868101 @default.
• W2024444204 cites W2313886795 @default.
• W2024444204 cites W2331774671 @default.
• W2024444204 cites W3146972477 @default.
• W2024444204 cites W3149162803 @default.
• W2024444204 cites W4361866922 @default.

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