结果显示，中国大陆地幔热流的空间分布不均匀。
Our result shows the nonuniform distribution of mantle heat flow in China.
其共同特征是：具明显的递增变质现象，以地幔热流上升为主要因素，构造背景为碰撞造山。
Their general characteristics are of obvious progressive metamorphism, with the heat flow from mantle as the essential factor and a collision orogenic belt to be the tectonic setting.
海盆区地幔热流在地表实测大地热流中所占比例高于80 %，地壳下部热流在地壳总热流中所占比例小于2 0 %。
The percentage of heat flow from mantle is bigger than 80% in terrestrial heat flow, whereas the percentage of lower crustal heat flow is smaller than 20% in terrestrial heat flow.
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