Výsledky vyhledávání - "Chao-Ming Xie"

RETRACTED-Late Permian to early Triassic gabbro in North Lhasa, Tibet: evidence for plume – subduction-zone interaction of the Palaeo-Tethys ocean

Autor: Meng-Long Duan, Chao-Ming Xie, Bin Wang, Yu-Hang Song, Wen-qing Li, Yu-jie Hao

Publikováno v: Geological Magazine. 160:393-408

The Palaeo-Mesozoic geodynamic evolution of the Tangjia–Sumdo accretionary complex belt, which separates the North and South Lhasa Terrane, remains controversial. Moreover, the lack of geological records restricts the understanding of the evolution

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::b7b0e213e7cbf01eacad727718ef8cd6
https://doi.org/10.1017/s0016756822001182

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Akademický článek

Opening of the Sumdo Paleo-Tethys Ocean and rifting of the Lhasa terrane from Gondwana: Insights from early Carboniferous magmatism in southern Tibet.

Autor: Bin Wang^1,2, Chao-Ming Xie^1,3,4 xcmxcm1983@jlu.edu.cn, Yakymchuk, Chris², Yong-Sheng Dong¹, Yu-Hang Song¹, Meng-Long Duan¹

Publikováno v: Geological Society of America Bulletin. Jan/Feb2024, Vol. 136 Issue 1/2, p531-546. 16p.

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Opening of the Sumdo Paleo-Tethys Ocean and rifting of the Lhasa terrane from Gondwana: Insights from early Carboniferous magmatism in southern Tibet

Autor: Bin Wang, Chao-Ming Xie, Chris Yakymchuk, Yong-Sheng Dong, Yu-Hang Song, Meng-Long Duan

Publikováno v: GSA Bulletin.

The late Paleozoic tectonic evolution of the Lhasa terrane and opening of the Sumdo Paleo-Tethys Ocean remain controversial due to limited data and the ambiguous tectonic significance of Paleozoic magmatism in the southern Lhasa subterrane. Here, we

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::72b188924abe491d844f1b2781dd827e
https://doi.org/10.1130/b36761.1

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Subduction–collision and exhumation of eclogites in the Lhasa terrane, Tibet Plateau

Autor: Yiming Liu, Runhua Guo, Chao-Ming Xie, Bin Wang, Yongjiang Liu, Yu-Chao Dong, Xianzhi Cao, Sanzhong Li, M. Santosh

Publikováno v: Gondwana Research. 102:394-404

The Tibet Plateau is a key region to understand the evolution of the Tethys Oceans. The finding of Permian–Triassic eclogites and Carboniferous–Triassic ophiolites indicated the existence of a Paleo–Tethys Ocean in the Lhasa terrane, although t

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::2d28eba9648154d3be7dd68a98c45d09
https://doi.org/10.1016/j.gr.2020.01.019

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Supplemental Material: Opening of the Sumdo Paleo-Tethys Ocean and rifting of the Lhasa terrane from Gondwana: Insights from early Carboniferous magmatism in Southern Tibet

Autor: null et al., Chao-Ming Xie, Bin Wang

Table S1: Representative magmatism of the Paleo-Tethys Ocean in the Qinghai-Tibet Plateau. Table S2: Whole-rock major (wt%) and trace element (ppm) data of the meta-basalt in Tangjia area (Tj20T09) and meta-gabbro in Sumdo area (Sd17T44) and trace el

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::23348a74b8b1a89626228636faa77096
https://doi.org/10.1130/gsab.s.22089425.v1

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Transition from oceanic subduction to continental collision recorded in the Bangong-Nujiang suture zone: Insights from Early Cretaceous magmatic rocks in the north-central Tibet

Autor: Wei Wang, Qingguo Zhai, Jin-Heng Liu, Pei-yuan Hu, Chao-Ming Xie, An-Bo Luo, Cai Li, Ming Wang

Publikováno v: Gondwana Research. 78:77-91

The transition from oceanic subduction to continental collision is a key stage in the evolution of ancient orogens. We present new data for Early Cretaceous diorite and granite porphyry from north–central Tibet to constrain the evolution of the Ban

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::6e13990c954b8153efc513b8d75695df
https://doi.org/10.1016/j.gr.2019.09.008

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Early Neoproterozoic granitic gneisses in the Amdo micro-continent, Tibet: petrogenesis and geodynamic implications

Autor: Bin Wang, Yu-Chao Dong, Yongsheng Dong, Chao-Ming Xie, Menglong Duan, Yuhang Song, Yun-Peng Yu

Publikováno v: International Geology Review. 63:342-356

The palaeogeographic locations of ancient continental blocks in the Tibetan Plateau, especially of micro-continental blocks during the Neoproterozoic supercontinent cycle, remain enigmatic. To clar...

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::871e61e094e39313c4c18d1898dca7de
https://doi.org/10.1080/00206814.2019.1710866

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