This process is called tectonic-metallogenesis.
这一过程被称为构造成矿作用。
The geodynamic regime of mantle-derived uranium metallogenesis and theory of hotspot uranium metallogenesis are briefly discussed.
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。
Outwards from the mantle uplift center, the metallogenesis becomes weaker, the deposit scale smaller and the ore-bearing horizon older.
该矿带具有自幔隆中心向外矿化渐弱、矿床规模变小、赋矿层位变老等规律。
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