研究结果表明,这些岩石的热导率值主要受控于其矿物成分,特别是石英的含量。
Studies demonstrate that the thermal conductivity of these rocks is mainly controlled by the contents of minerals, especially by the quartz content.
分维值还与断层泥的母岩、厚度、粘土矿物含量和所处的断裂部位等相关。
The fractal dimension value is also relative with parent rock, thickness, structural position and clay content of the fault gouge.
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