The Dashui Subduction Complex in the Eastern Tianshan-Beishan Orogen (NW China): Long-Lasting Subduction-Accretion Terminated by Unique Mid-Triassic Strike-slip Juxtaposition of Arcs in the Southern Altaids

Name: The Dashui Subduction Complex in the Eastern Tianshan-Beishan Orogen (NW China): Long-Lasting Subduction-Accretion Terminated by Unique Mid-Triassic Strike-slip Juxtaposition of Arcs in the Southern Altaids
Creator: Kai Wang
Published: 2022-05-26T14:15:46.169Z
Keywords: Tectonics, Geological Mapping, Provenance Analysis, Structural Analysis

Wang, Kai; Xiao, Wenjiao; Windley, Brian F.; Mao, Qigui; Ji, Wenhua; Sang, Miao; Huang, Peng; Wang, Ping

doi:10.17632/tgxvx8wb7d.3

The Dashui Subduction Complex in the Eastern Tianshan-Beishan Orogen (NW China): Long-Lasting Subduction-Accretion Terminated by Unique Mid-Triassic Strike-slip Juxtaposition of Arcs in the Southern Altaids

Published: 26 May 2022| Version 3 | DOI: 10.17632/tgxvx8wb7d.3

Contributors:

Kai Wang, Wenjiao Xiao, Brian F. Windley, Qigui Mao, Wenhua Ji, Miao Sang, Peng Huang, Ping Wang

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Supporting Information for[The Dashui subduction complex in the Eastern Tianshan-Beishan Orogen (NW China): Long-lasting subduction-accretion terminated by unique mid-Triassic strike-slip juxtaposition of arcs in the southern Altaids]

The Dashui Subduction Complex in the Eastern Tianshan-Beishan Orogen (NW China): Long-Lasting Subduction-Accretion Terminated by Unique Mid-Triassic Strike-slip Juxtaposition of Arcs in the Southern Altaids

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