The Dashui accretionary 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 accretionary 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: 2021-12-16T15:58:10.275Z
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.1

The Dashui accretionary 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: 16 December 2021| Version 1 | DOI: 10.17632/tgxvx8wb7d.1

Contributors:

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

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The Dashui accretionary 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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