Petrology, geochemistry, and metamorphic evolution of meta-sedimentary rocks in the Diancang Shan-Ailao Shan metamorphic complex, Southeastern Tibetan Plateau
A four-stage clockwise P–T path with near-isothermal decompression has been established.
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The Diancang Shan–Ailao Shan complex belt record a geodynamic process related to subduction–collision–exhumation between the Yangtze and Indochina plates.