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Southward trench migration at ~130-120 Ma caused accretion of the Neo-Tethyan forearc lithosphere in Tibetan ophiolites
Qing Xiong*, William L. Griffin, Jian Ping Zheng, Suzanne Y. O'Reilly, Norman J. Pearson, Bo Xu, Elena A. Belousova
*Corresponding author for this work
Research output: Contribution to journal › Article › peer-review
133
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(Scopus)