The Western Tianshan high-pressure metamorphic rocks occur within the greenschist facies country rocks as small discrete blocks, lenses, bands, laminae or intercalated slabs.

 
  • 摘要西天山高压变质岩呈不连续岩块、凸镜体、条带、薄层或夹层岩片产于绿片岩相围岩中。
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