二郎坪群蛇绿岩中多金属矿床属火山成因块状硫化物矿床。
The poly metallic deposit occurred in the Erlangping ophiolite of eastern Qinling Mountain was regarded as volcanogenic type.
东秦岭二郎坪群蛇绿岩中广泛发育火山成因块状硫化物矿床。
Volcanogenic massive sulfide deposits occur widely in the ophiolite of the Erlangping Group of the Eastern Qinling Mountains.
火山演化从早期到中晚期分别形成铁矿层、火山成因块状硫化物矿床和黄铁矿化层。
Early to late stage volcanic evolution resulted in the formation of iron formations, sulfide deposits and pyrite mineralization beds.
研究了北祁连山造山带火山成因块状硫化物矿床（VMS）类型、金属来源与容矿围岩、火山岩类型及其构造环境的关系。
The relationships between VMS types, source of metal, host rock, volcanic rock types and tectonic setting have been studied in this paper.
同时还介绍了阿舍勒火山成因块状硫化物铜-锌矿床的地质、物、化探找矿模型，可供同类矿床成矿预测参考。
The geological and geophysical prospecting models were also introduced for reference to massive sulphide Cu - Zn deposits of volcanic origin in Ashele.
同时还介绍了阿舍勒火山成因块状硫化物铜-锌矿床的地质、物、化探找矿模型，可供同类矿床成矿预测参考。
The geological and geophysical prospecting models were also introduced for reference to massive sulphide Cu - Zn deposits of volcanic origin in Ashele.
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