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地温勾配 逆転

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Temperature profile of inner Earth, schematic view (estimated). The red dashed line shows the minimum temperature for the respective mantle rock to melt. The geothermal gradient remains below the melting temperature of the rock, except in the asthenosphere. Sharp rises occur in the uppermost mantle and at the core–mantle boundary.

地温勾配の仕組みと地球内部の熱源エネルギーの源泉を探る

地温勾配地球内部熱放射性崩壊地熱エネルギー
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