Cenozoic evolution of the Altyn Tagh and East Kunlun fault zones inferred from detrital garnet, tourmaline and rutile in southwestern Qaidam Basin (Northern Tibetan Plateau)

Publisher： John Wiley & Sons Inc

E-ISSN： 1365-2117|30|1|35-58

ISSN： 0950-091x

Source： BASIN RESEARCH, Vol.30, Iss.1, 2018-02, pp. : 35-58

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