The ore structure and generation of cobalt-gold ore minerals suggest that their formation mainly related to submarine sedimentary exhalation, reformed and mobilized in late collision orogenesis.
钴（金）矿石组构及矿石矿物的世代显示其主要与海底喷气沉积成矿作用有关，在后期的碰撞造山过程中，受到了改造和活化。
They occurred under the tectonic setting ranging from post collision uplift to late orogenesis.
产生于板块碰撞后隆起到造山晚期的构造背景。
They occurred under the tectonic setting ranging from post collision uplift to late orogenesis.
产生于板块碰撞后隆起到造山晚期的构造背景。
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