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喀拉通克铜镍硫化物矿床的岩浆深渊熔离—贯入及其形成力学机理
引用本文:黄继钧.喀拉通克铜镍硫化物矿床的岩浆深渊熔离—贯入及其形成力学机理[J].矿物岩石,1990(4).
作者姓名:黄继钧
作者单位:成都地质学院 成都
摘    要:通过新疆喀拉通克铜镍硫化物矿床、矿体地质特征和岩浆深渊熔离—贯入特征的研究,提出“动—静—动—静”交替作用的力学机制,指出该铜镍硫化物矿床为岩浆深渊熔离—贯入成因,使小岩体有赋存大矿的可能性。

关 键 词:铜镍硫化物矿床  重力分异  结晶分异  岩浆深渊熔离  构造应力躯动

MAGMA SEGREGATION-MAGMA INJECTION AND FORMING MECHANISM OF KELATONGKE COPPER-NICKEL SULFIDE ORE DEPOSIT
Huang Jijuen.MAGMA SEGREGATION-MAGMA INJECTION AND FORMING MECHANISM OF KELATONGKE COPPER-NICKEL SULFIDE ORE DEPOSIT[J].Journal of Mineralogy and Petrology,1990(4).
Authors:Huang Jijuen
Abstract:The paper introduces the geological characteristics of the ore deposit and ore bodies, and the characteristics of magma segregation-magma injection. It indicates a mechanism of alternate action of "Active-calm-Active-calm" and pointes out the cause of formation of magma segregation-magma injection in the copper-nickel sulfide ore deposits. Hence, it is possible to make small bodies to stick into huge ore deposits.
Keywords:copper-nickel sulfide ore deposits  heavy force differentiation  crystallization differentiation  magma segregation  constructional suitable force drive
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