The lithosphere thickness and bottom temperature of this region have been derived by making use of the averaged heat flow of the four regions.
并用四个地区的平均热流值推导出该区的岩石圈厚度和底部温度。
Present geothermal gradient and geothermal flux of the Ordos basin is controlled by the thickness of the earth crust in the different tectonic element and the thickness of lithosphere.
鄂尔多斯盆地现今地温梯度与大地热流的展布受盆地不同构造单元地壳厚度、岩石圈厚度变化控制。
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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