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Copper-Polymetal Metallogenic Series and Prospecting Perspective of Eastern Section of Gangdise

机译:冈底斯东段铜多金属成矿系列及找矿前景

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摘要

Geological, geophysical, geochemical and remote sensing comprehensive studies show that big ore-prospecting potentiality is contained in the eastern section of the Gangdise Mountains, Tibet. There are various mineralization types with dominant types of porphyry and exhalation. According to their relations with tectonic evolution, they are divided into four kinds of metallogenic series as follows: magmatic type (Cr, Pt, Cu, Ni) and exhalation type (Cu, Pb, Zn, Ag) ore deposit series related to Neo-Tethys oceanic crust subduction action (125―96 Ma) ; epithermal type (Au, Ag, Pb, Zn, Sb), altered fractured rock type (Cu, Mo) and skarn rock type (Cu) ore deposit series related to arc-continental collision; porphyry type (Cu, Mo), cryptoexplosion breccia type (Cu, Au, Pb, Zn), shear zone type (Au, Ag, Sb) and skarn rock type (Cu, Fe) ore deposit series with relation to post-orogenic exten-sional strike-slip. From subductive complex to the north, zoning appears to be crystallization differentiation type (segregation type)-shear zone type (altered rock type)-skarn rock type, epithermal type-porphyry type-porphyry type and exhalation type-exhalation type-hydrothermal filling-replacement type. The ore deposit is characterized by multi-places from the same source, parity and multi-stage, hypabyssal rock from the deep source and poly genetic compound as a whole.
机译:地质,地球物理,地球化学和遥感综合研究表明,西藏冈底斯山脉东部蕴藏着巨大的找矿潜力。有多种矿化类型,斑岩和呼出气占优势。根据其与构造演化的关系,将其分为与新近纪有关的岩浆型(Cr,Pt,Cu,Ni)和呼出型(Cu,Pb,Zn,Ag)矿床系列四种。特提斯洋壳俯冲作用(125〜96 Ma);与弧-陆碰撞有关的超热型(Au,Ag,Pb,Zn,Sb),蚀变岩型(Cu,Mo)和矽卡岩型(Cu)矿床系列;与造山后延伸有关的斑岩型(铜,钼),隐爆角砾岩型(铜,金,铅,锌),剪切带型(金,银,锑)和矽卡岩型(铜,铁)矿床系列-部分走滑。从俯冲带到北部,地带似乎是结晶分化型(偏析型)-剪切带型(变岩型)-矽卡岩型,超热型-斑岩型-斑岩型和呼气型-呼气型-水热充填型。替换类型。矿床的特征是来自同一源头的多个地方,来自深部源头的奇偶校验和多阶段的海底岩石以及整个多遗传化合物。

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