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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.
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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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