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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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]
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2024-01-31
