| 喀拉通克1号铜镍硫化物矿床研究 |
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| 引用本文： | 赵昌龙.喀拉通克1号铜镍硫化物矿床研究[J].新疆地质,1991(3). |
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| 作者姓名： | 赵昌龙 |
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| 作者单位： | 新疆维吾尔自治区地质矿产局第四地质大队 |
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| 摘 要： | 本文通过大量的测试研究.对喀拉通克1号铜镍硫化物矿床的围岩、构造、岩石矿物,矿石及同位素地质等特征进行了详细的阐述.该矿是由上地幔亚碱性拉斑玄武岩浆经中间岩浆房液态层状分异后,侵位于活动区,其中的含矿岩浆就地熔离成矿,同源矿浆贯入成矿,以及它们复合定位所形成的岩浆熔离叠生矿床.并建立起该矿床的成岩成矿模式.
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| 关 键 词： | 喀拉通克 铜镍硫化物 矿床成因 成岩成矿模式 |
ON KARATUNGKE No.1 Cu-Ni SULPHIDE DEPOSIT |
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| Zhao Changlong.ON KARATUNGKE No.1 Cu-Ni SULPHIDE DEPOSIT[J].Xinjiang Geology,1991(3). |
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| Authors: | Zhao Changlong |
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| Abstract: | Through tremendous studies on Karatungke No.l Cu-Ni sulphide deposit, the characteristics of countryrock, structure, petrology and mineralogy, ores and isotopic geology are described in details in this paper. This deposit was formed by repeated melting and dissociating of ore magma with composite emplacement which came from sub-alkalic tholeiite of upper mantle undergoing stratiform differentiation in a liquid state in the middle magma house and intruding into the active zone. Its diagenetic and minerogenetic models are also built up. |
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| Keywords: | Karatungke Cu-Ni sulphide origin of ore deposit diagenetic and mineroge-netic models |
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