摘要
大坪钒矿床,为下寒武统黑色岩系中的沉积钒矿床。本文在论述矿床地质特征的基础上,对矿床的成因进行了详尽的分析。从钒的赋存状态、成矿物质来源、有机地球化学作用论证了该矿床应属生物化学沉积矿床,并阐明了成矿作用机制。
The Daping Varadium-Deposit is a sedimentary Varadium-Depossit formed Low cambrian black rock series.The ore-bed occurs with stratiform and sililar stratiform and its occurrence is stable.In ore-bed concretions developed,and associated elements are P,Ni,Mo,Pt etc.From study on occuring state of Varadium, source of minerogenetic matter,organic geochemical process,and minerogenetic process,the deposit is a biochemical sedimentary deposit.
出处
《湘潭矿业学院学报》
1989年第2期129-134,共6页
Journal of Xiangtan Mining Institute
关键词
钒矿床
矿床地质
成矿
Varadium-deposit
organic geochemical process
minerogenetic cause of formation
geological characteristic of deposit
