| 新疆喀拉通克矿区I号含贵金属硫化铜镍矿床的成岩成矿模式 |
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| 引用本文： | 潘长云,王润民.新疆喀拉通克矿区I号含贵金属硫化铜镍矿床的成岩成矿模式[J].矿床地质,1992,11(2):113-124. |
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| 作者姓名： | 潘长云 王润民 |
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| 作者单位： | 云南省地质科学研究所 |
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| 摘 要： | 讨论了喀拉通克矿区I号含贵金属硫化铜镍矿床含矿岩体及矿体地质特征、成岩成矿物质来源和成矿作用等，建立了相应的成岩成矿模式。该模式认为，喀拉通克I号含贵金属硫化铜镍矿床是一叠生矿床，它是由深部熔离作用形成的富含硫化物的含矿岩浆，侵位后经就地熔离成矿怍用、纯硫化物矿浆就地结晶和挤压迁移作用以及热液成矿作用形成的，矿床类型属岩浆熔离型。
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| 关 键 词： | 成岩 成矿 铜矿 镍矿 矿床 |
Petrogenic And Metallogenic Model Of The No. 1 Precious Metal-Bearing Copper-Nickel Sulfide Deposit In The Kalatongke Ore District, Xinjiang |
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| Abstract: | This paper deals with geological characteristics of the ore-bearing intrusive body and the ore body, petrogenic and metallogenic substances and mineralization types of the No. 1 precious metal-bearing copper-nickel sulfide deposit in the Kalatongke ore district. On such a basis, a corresponding petrogenic and metallogenic model is established. The model holds that the ore deposit is a telescoped one formed by in-situ liquation mineralization, crystallization and compressional migration of pure sulfide ore magma generated through insitu liquation and hydrothermal ore-forming process after the emplacement of sulfide-rick magma formed by deep liquation. It is thus concluded that the ore deposit is of magmatic liquation type. |
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