盆地热历史类型受其地球动力学背景及构造演化史控制。
The thermal history type of basin is controlled by its dynamic background of the earth and structural evolution.
文章扼要阐述了幔源铀成矿的地球动力学背景，评述了热点铀成矿理论。
The geodynamic regime of mantle-derived uranium metallogenesis and theory of hotspot uranium metallogenesis are briefly discussed.
也就是说，燕山运动是东亚构造体制转变的产物，其出现有着深刻的地球动力学背景。
That is, the Yanshan Movement is the result of the conversion of tectonic regimes in East Asia, which has profound global geodynamic Settings.
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