Some Remarks about Geothermal Gradient of Sedimentary Basins
沉积盆地地温梯度研究中应注意的问题
The present geothermal gradient of the Huh Lake depression is 3.
呼和湖凹陷现今地温梯度为3。
It has discussed the distributing disciplinarian and controlling factors of geothermal gradient.
计算了地温梯度，探讨了分布规律和控制因素。
The next step is to infer the calcite precipitation time by the geothermal gradient and burial history.
再由地温梯度和埋藏史资料，判断方解石沉淀的时间。
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