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• W2912140369 abstract "The Late Palaeozoic Solonker‐Xar Moron‐Changchun‐Yanji Suture (SXCYS) is considered to mark the location of the final closure of the Paleo‐Asian Ocean, which separated the North China Craton to the south and the amalgamated blocks to the north in Northeast China. There has always been controversy about its eastern extension in Northeast China and the final closure time of the Paleo‐Asian Ocean. To explore this issue, we collected gabbro and quartz‐diorite samples in the Hunchun area for the genesis of mafic magma and age dating, and five groups of Permian to Triassic sandstones belonging to both sides of the potential suture locations in the middle and east Jilin Province for the provenance analysis to discuss the final closure time of the Paleo‐Asian Ocean and the possible positions of the eastward termination of the SXCYS. The gabbro reveals a Middle Permian concordia average age of 266.9 ± 5.2 Ma, and the quartz diorite reveals a Late Permian Concordia average age of 258.8 ± 4.8 Ma. Lithological and geochemical analysis reveal the two rock samples belong to low‐K arc tholeiites from the oceanic island and calk‐alkaline volcanics from the active continental margin, respectively, which implies that during the middle to late Permian, the SW margin of the Jiamusi–Khanka Block (JB) continuously experienced the subduction process from the Paleo‐Asian Ocean Plate. The final closure time of the Paleo‐Asian Ocean should be later than the Late Permian. Meanwhile, four groups of sandstone from the east Jilin reveal typically Jiamusi–Mongolia Block (JMB) provenance features, with age components of ~500 Ma, ~0.9–1.5 Ga implying that the Wangqing, Hunchun, Kaishantun area belongs to the northern part of the SXCYS from late Early Permian to Middle Triassic, with youngest age components of 288.2 ± 2.8, 275.5 ± 1.8, 250 ± 1.7, and 244.9 ± 1.7 Ma, respectively. The late Early Permian sandstone from the middle Jilin reveals the youngest age component of 273.8 ± 3.4 Ma and the age component of 487 ± 3 Ma also revealing JMB feature. Comparing to previous studies, we propose that the Paleo‐Asian Ocean finally closed during Middle to Late Triassic. A possible ENE fault separates the eastern extension of SXCYS into two parts, which means the possible position of the eastward extension of the SXCYS should go along the Wangqing‐Kaishantun with NNW direction in the west, Hunchun‐Laoheishan with NW direction in the east." @default.
• W2912140369 created "2019-02-21" @default.
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• W2912140369 date "2019-02-14" @default.
• W2912140369 modified "2023-10-01" @default.
• W2912140369 title "Eastern extension of the Solonker‐Xar Moron‐Changchun‐Yanji Suture Zone: Constraints from thermochronology of sedimentary and mafic rocks in the Hunchun‐Yanji area, Northeast China" @default.
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• W2912140369 cites W1518712899 @default.
• W2912140369 cites W1966297169 @default.
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• W2912140369 cites W1973675853 @default.
• W2912140369 cites W1975042776 @default.
• W2912140369 cites W1977431633 @default.
• W2912140369 cites W1978904154 @default.
• W2912140369 cites W1984329251 @default.
• W2912140369 cites W1990701109 @default.
• W2912140369 cites W1991218568 @default.
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• W2912140369 cites W2003348019 @default.
• W2912140369 cites W2005520120 @default.
• W2912140369 cites W2006066004 @default.
• W2912140369 cites W2008127132 @default.
• W2912140369 cites W2009732140 @default.
• W2912140369 cites W2013747285 @default.
• W2912140369 cites W2019034794 @default.
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• W2912140369 cites W2026420692 @default.
• W2912140369 cites W2030154085 @default.
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• W2912140369 cites W2072664369 @default.
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• W2912140369 cites W2073964263 @default.
• W2912140369 cites W2075018281 @default.
• W2912140369 cites W2078816109 @default.
• W2912140369 cites W2080214030 @default.
• W2912140369 cites W2084163522 @default.
• W2912140369 cites W2087662765 @default.
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• W2912140369 cites W2091304021 @default.
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• W2912140369 doi "https://doi.org/10.1002/gj.3462" @default.
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