Metamorphic Characteristics and Tectonic Implications of the Kadui Blueschist in the Central Yarlung Zangbo Suture Zone, Southern Tibet

Guangming Sun; Xu-Ping Li; Wenyong Duan; Shuang Chen; Zeli Wang; Lingquan Zhao; Qingda Feng

doi:10.1007/s12583-018-0854-9

Volume 29 Issue 5

Oct 2018

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Journal of Earth Science > 2018 > 29(5): 1026-1039.

Guangming Sun, Xu-Ping Li, Wenyong Duan, Shuang Chen, Zeli Wang, Lingquan Zhao, Qingda Feng. Metamorphic Characteristics and Tectonic Implications of the Kadui Blueschist in the Central Yarlung Zangbo Suture Zone, Southern Tibet. Journal of Earth Science, 2018, 29(5): 1026-1039. doi: 10.1007/s12583-018-0854-9

Citation:

Guangming Sun, Xu-Ping Li, Wenyong Duan, Shuang Chen, Zeli Wang, Lingquan Zhao, Qingda Feng. Metamorphic Characteristics and Tectonic Implications of the Kadui Blueschist in the Central Yarlung Zangbo Suture Zone, Southern Tibet. Journal of Earth Science, 2018, 29(5): 1026-1039. doi: 10.1007/s12583-018-0854-9

Citation:

Guangming Sun, Xu-Ping Li, Wenyong Duan, Shuang Chen, Zeli Wang, Lingquan Zhao, Qingda Feng. Metamorphic Characteristics and Tectonic Implications of the Kadui Blueschist in the Central Yarlung Zangbo Suture Zone, Southern Tibet. Journal of Earth Science, 2018, 29(5): 1026-1039. doi: 10.1007/s12583-018-0854-9

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Metamorphic Characteristics and Tectonic Implications of the Kadui Blueschist in the Central Yarlung Zangbo Suture Zone, Southern Tibet

doi: 10.1007/s12583-018-0854-9

1.
Shandong Provincial Key Laboratory of Depositional Mineralization and Sedimentary Minerals, Shandong University of Science and Technology, Qingdao 266590, China
2.
Institut für Geologie, Mineralogie und Geophysik, Ruhr-Universität, Bochum 44780, Germany
3.
Center of Hydrogeology and Environmental Geology Survey, China Geological Survey, Baoding 071051, China

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Corresponding author: Xu-Ping Li
Received Date: 20 May 2018
Accepted Date: 27 Jul 2018
Publish Date: 01 Oct 2018

Abstract

Abstract

The Kadui blueschist is located in the central section of Yarlung Zangbo suture zone (YZSZ), southern Tibet, and has been subjected to the subduction of the Neo-Tethyan Ocean below the Asian Plate and provides important clues for better understanding the evolution of the India-Asia convergence zone. In this paper, the systematical petrographic and mineral chemical studies were carried out on the Kadui blueschist, which reveal a mineral assemblage of sodic amphibole, chlorite, epidote, albite and quartz with accessory minerals of titanite, calcite and zircon. Electron microprobe analyses demonstrate that amphibole shows zoned from actinolite core to ferrowinchite/riebeckite rim composition indicating that the sodic amphibole has formed during a prograde metamorphic event. The protolith of the blueschist is an intermediate-basic pyroclastic rock. The calculated pseudosection indicates a clockwise P-T path and constrains peak metamorphic conditions of about 5.9 kbar at 345℃. This condition is transitional between pumpellyite-actinolite, greenschist and blueschist facies with a burial depth of 20-22 km and a thermal gradient of 15-16℃/km. This thermal gradient belongs to high pressure intermediate P/T facies series and is possibly related to a warm subduction setting of young oceanic slabs. Our new findings indicate that the Kadui blueschist in the central part of YZSZ experienced a rapid subduction and exhumation process as a response to a northward subduction of the Neo-Tethyan oceanic lithosphere during the initial India-Asia collision stage.
- Kadui blueschist,
- metamorphism,
- P-T conditions,
- accretionary complex,
- southern Tibet

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References(101)

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