通过对湖南沃溪矿床的宏观至微观尺度上的矿石组构学研究，揭示出矿床系同生热水沉积成因。
Ore fabric studies of the Woxi W_Sb_Au deposit on macro_ to micro_ scales have revealed that the deposit is of syngenetic hydrothermal sedimentary origin.
蔷薇辉石矿床的形成主要经历了沉积期和区域变质期两大阶段。 成因类型属变质岩型低温变质相蔷薇辉石矿床。
The rhodonite deposit was for- med mainly through two stages, sedimentation and regional metamorphism, and its genetic type belongs to epithermal metamorphic facies.
毒重石矿床属热水沉积成因层控矿床。
Witherite deposits belong to stratabound deposits of hot water sedimentation.
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