The thermal weakening of crust/mantle rocks induced by heat represents a main way in rock weakening,which provides material condition for intracontinental deformation.
由热引起的地壳/地幔岩石材料的热弱化是弱化的主要途径,为陆内变形准备了物质条件。
参考来源 - 岩石圈HPE热弱化与陆内构造变形·2,447,543篇论文数据,部分数据来源于NoteExpress
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