【摘要】 早寒武世黑色岩系中,蕴藏丰富的金属和非金属矿产。杨子板块北缘的南秦岭褶皱带下寒武统钒矿床,具矿层形态简单,埋藏浅,储量大的特点。鄂西北尤以武当山—大别山早古生代海相黑色页岩杨家堡式钒矿床为典型,火星庙钒矿床赋矿层位与其一致,为南秦岭下寒武统庄子沟组黑色岩系。以多年野外工作数据为基础,通过对火星庙钒矿床、区域地质特征、矿区地质及构造特征以及矿体特征的详细论述,阐明火星庙钒矿为受向斜构造控制的生物化学沉积变质改造型钒矿床。更多还原

【Abstract】 In the Early Cambrian black rock series,there are richful of metal and non-metallic mineral resources.The Lower Cambrian vanadium deposit in the South Qinling fold belt on the north margin of the Yangzi plate has the characteristics of simple shape of ore layer,shallow burial depth and large scale reserves.Yangjiabao-type vanadium deposit hosted in the early Paleozoic marine black shale is especially a typical representative in the Wudang Mountain-Dabie Mountain area of the northwestern Hubei.The ore-bearing stratum of Hushenmiao vanadium deposit is consistent with that of the former deposit,in which there is a set of black rock series of the Lower Cambrian Zhuangzigou Formation in the South Qinling.According to the field work data in many years,on the basis of regional and geological characteristics,geological and structural characteristics of the mining area,and ore body characteristics,the article has clarified that the Huoxingmiao vanadium deposit is a biochemical sedimentary metamorphism alteration type vanadium deposit,which is controlled by the syncline structure.更多还原