首页> 中文期刊> 《西南科技大学学报》 >贵州遵义新土沟镍钼矿地质特征及成因浅析

贵州遵义新土沟镍钼矿地质特征及成因浅析

         

摘要

The Xintugou area the lower Cambrian black is widely distributed contains rich mineral resources , including Ni-Mo resources particularly rich. Ni - Mo ore bodies occur in the lower Cambrian cattle shoe pond group of black charcoal clay rock, Ni 2. 68% - 7. 30% (mean 4. 12% ), Mo 4. 80% -8.67% (mean 6. 81% ). Ore major types of carbonaceous mudstone type nickel, molybdenum, nickel, molybdenum pyrite type. Through the source of ore-forming materials, organic geochemical action research , preliminary that Xintugou nickel molybdenum for marine chemistry and biochemistry sedimentary formation, deposit origin should be bottom spray deposition.%新土沟地区下寒武统黑色岩系分布广泛,蕴含着丰富的矿产资源,其中镍钼矿资源尤为丰富.镍钼矿体赋存于下寒武统牛蹄塘组的黑色炭质黏土岩中,镍含量2.68%~ 7.30%,平均品位4.12%;钼含量4.80%~8.67%,平均品位6.81%.矿石主要类型为黄铁矿型镍、钼矿和炭质泥岩型镍、钼矿.通过对成矿物质来源、成矿作用的研究,初步认为新土沟镍钼矿为海相化学及生物化学沉积生成,矿床成因应为海底喷流沉积成因.

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