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地球近地表平均地温梯度为3℃/100m,大气降水渗入地下,从地下深处的岩石中吸取热量,再沿着适当的断裂或裂隙通道返回地表...
地球近地表平均地温梯度为3℃/100m,大气降水渗入地下,从地下深处的岩石中吸取热量,再沿着适当的断裂或裂隙通道返回地表
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地球近地表平均地温梯度为3℃/100m,大气降水渗入地下,从地下深处的岩石中吸取热量,再沿着适当的断裂或裂隙通道返回地表,译文:The average geothermal gradient of the Earth's near-surface 3 ℃ / 100m, meteoric water into the ground to absorb heat from deep underground rock, and then returned to the surface along the fracture or fissure channel
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The earth near-surface average geothermal gradient for 3 ℃ / 100 m, atmospheric precipitation infiltration underground, from deep underground rock absorb heat, then along the appropriate fracture or crack channel to return to the surface
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