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广义地说地热和地震活动性之间的关系是很不清楚的。这种关系可以用几种方法来了解。一种方法是地震能量密度图(例如以每100年耳格/公里~2计算),同水平地热梯度相对比,象 Cermak 等(1975)所表示的那样。在这个情况下,应将相同深度水平的地热和地震参数进行对比,计算地震震中深度上的水平地热梯度。根据上述工作结果,这种条件不是很清楚的。第二个方法是将地热图同地震能量密度图对比。通常是这样做,但很概括,所以其
Broadly speaking, the relationship between geothermal and seismicity is unclear. This relationship can be understood in several ways. One method is the seismic energy density map (for example, calculated at 100 km / km2), as opposed to a horizontal geothermal gradient, as shown by Cermak et al. (1975). In this case, geothermal and seismic parameters of the same depth level should be compared to calculate the horizontal geothermal gradient at the epicentral depth of the earthquake. According to the above work results, this condition is not very clear. The second method is to compare the geothermal map with the seismic energy density map. This is usually done, but very general, so it’s