节点文献
黄山铜镍硫化物矿床10号矿体形成机理及远景评价
METALLOGENIC MECHANISM AND PROSPECTIVE VALUE FOR NO. 10 OREBODYIN HUANGSHAN Cu-Ni SULFIDE DEPOSIT
【摘要】 黄山铜镍矿床10号矿体是赋存在镁铁—起镁铁杂岩体内辉长苏长岩相中的浅富铜镍矿体,它是由含有高温气态的硫化物熔浆贯入—硫化作用成矿。矿体形成后受到成矿后断层的破坏。
【Abstract】 NO. 10 orebody in Huangshan Cu-Ni sulfide deposit, Xinjiang,is an enriched and outcropped one located in the gabbonorite of Huangshan mafic-ultramafic complex. The orebody was formed by the injection and sulfidization of the remnant sulfide melt with high-temperature gaseous sulfur,and was faulted afterwards.
- 【文献出处】 矿物岩石 ,JOURNAL OF MINERALOGY AND PETROLOGY , 编辑部邮箱 ,1996年01期
- 【分类号】P618.410.1
- 【被引频次】4
- 【下载频次】108