The formation the LILE-rich amphibolite is resulted from the LILE-rich hydrothermal fluid emplacement, which provide the material source for the Kuerti plagiogranite formation.

  • 由于受富含轻稀土等大离子亲石元素的热水流体的交代,形成了富集大离子亲石元素的角闪岩。
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