The present geothermal field is controlled by thickness of lithosphere, structural features as well as groundwater activity.
现今地温场主要受岩石圈厚度、构造特征和地下水活动的影响。
The present geothermal field is controlled by thickness of lithosphere, structural features as well as groundwater activity.
现今地温场主要受岩石圈厚度、构造特征和地下水活动的影响。
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