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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Kai Wang
