It can be distinguished from the unmetamorphosed Mesozoic granite and the low pressure gneiss by the features: ( 1) the key metamorphic minerals: phengite and coronal garnet around albite;

  • 它以其下列特征与本区未变质花岗岩和围绕它的低压花岗质片麻岩相区别:(1)有标型矿物多硅白云母和长石的石榴石反应边;

  • 互联网摘选 2025-01-20 13:03:05

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