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.

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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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