D. Xin
6 Papers
D. Xin is an academic researcher. The author has contributed to research in topics: Geology & Subduction. The author has an hindex of 1, co-authored 1 publications.
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Papers
Two plutonic complexes of the Sanandaj-Sirjan magmatic-metamorphic belt record Jurassic to Early Cretaceous subduction of an old Neotethys beneath the Iran microplate
T.N. Yang,Jian-Lin Chen,Jian-Lin Chen,M.J. Liang,D. Xin,Mehraj Aghazadeh,Zengqian Hou,H.R. Zhang +7 more
TL;DR: In this paper, the Alvand and Qory plutonic complexes of SW Iran have been analyzed using LA-ICP-MS U/Pb analyses, along which the concordant age increase gradually from 120 to 190 Ma.
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Complete deformation history of the transition zone between oblique and orthogonal collision belts of the SE Tibetan Plateau: Crustal shortening and rotation caused by the indentation of India into Eurasia
M.J. Liang,Tiannan Yang,Chuan-Dong Xue,D. Xin,Zhen Yan,Cheng Liao,Xue Han,Zhipeng Xie,Kun Xiang +8 more
TL;DR: In this paper , the authors reconstructed the complete crustal deformation history of the oblique collisional belt, which consists of early and late stages of crustal shortening separated by a middle stage involving the ∼80° clockwise rotation of the crust.
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Multiple volcanic episodes of the Kermanshah forearc basin, SW Iran: a record of the deactivation and re-initiation of Neotethyan subduction involving a mid-oceanic ridge
TL;DR: In this article , the Kermanshah forearc basin was identified as the starting point of the Neotethyan Ocean between the Iranian and Arabian continents, which is filled with two terrestrial volcaniclastic successions separated by an Upper Cretaceous reef-facies limestone.
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Petrogenesis of the Late Eocene to Early Oligocene Yao'an Shoshonite Complex, Southeastern Tibet: Partial Melting of an Ancient Continental Lithospheric Mantle Beneath the Yangtze Block
TL;DR: In this article , the Yao'an Shoshonite complex (YSC) was found to be formed by partial melting of an ancient continental lithospheric mantle beneath the Yangtze block, which separates the orthogonal and oblique collision belts of the India-Eurasia collision orogen.
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Coherent chemical variation trends of the 55–25 Ma magmatic rocks in SE Tibet: N–S direction lithospheric stretching of Eurasia during early stage of India–Eurasia collision
Tiannan Yang,Mengmeng Dong,Chuan-Dong Xue,D. Xin,M.J. Liang +4 more
- 13 Sep 2023
TL;DR: The magmatic rocks in SE Tibet exhibit coherent chemical variation trends, reflecting the heterogeneous mantle and crusts of Eurasia and the NNW–SSE direction lithosphere stretching.
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