宏观碎裂结构与微观糜棱状结构是断层构造岩的主要特点。
The tectonites are characterized by macroscopic cataclastic and microscopic mylonitic structures.
哀牢山—金沙江构造带糜棱状花岗岩位于哀牢山深变质带中部。
Mylonitized granite in the AilaoshanJinshajiang tectonic zone is hosted in the center of the Ailaoshan high grade metamorphic belt.
哀牢山—金沙江构造带糜棱状花岗岩位于哀牢山深变质带中部。
Mylonitized granite in the AilaoshanJinshajiang tectonic zone is hosted in the center of the Ailaoshan high grade metamorphic belt.
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