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中文摘要：
文章进一步提出中国小岩体镍铜(铂族)矿床产出于三种地质背景,即古大陆内的小侵入体、造山带内小侵入体和与大陆溢流玄武岩有关的小侵入体,分别介绍了金川、喀拉通克和白马寨三个典型矿床的地质情况。从成矿的三个必要条件(①岩浆应达到硫化物饱和;②硫化物与岩浆之间应有足够的质量比;③硫化物聚集到有限的空间成矿)出发,结合矿床实例,阐述了成矿的深部过程和深部熔离-贯入成矿模式。论述了不同尺度的区域成矿规律:①三种地质背景;②邻近深大断裂;③三种岩体-矿床的分布结构形式;④矿集区往往是由一个同源多期次上侵的岩体群组成;⑤矿床由含矿岩浆上侵的终端岩浆房组成;⑥含矿岩浆贯入成矿往往伴随一定的流动分异作用或重力分异作用。
英文摘要：
Results of research indicate that Ni-Cu(PGE)ore deposits hosted in small intrusions in China mainly occur in three geologic settings:(1)within paleo-continents,(2)in orogenic belt,and(3)continental rift system such as the Panxi Rift system where a large number of flood basalts and associated mafic-ultramafic intrusive are present.Typical examples of these ore deposits are Jinchuan,Karatungk,Baimazhai,respectively.Based on three controlling factors:(1)sulfide saturation in magma,(2)enough mass ratio between ...
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Genesis of Concealed Cu-rich Ore Body in the Jinchuan Deposit, Northwestern China, and Its Prospecti
Compositional variations of olivine, clinopyroxene, plagioclase and apatite in the Panzhihua Fe-Ti-V
A new genetic model for the giant Ni-Cu-PGE sulfide deposits associated with the Siberian flood basa
Precise U–Pb zircon–baddeleyite age of the Jinchuan sulfideore-bearing ultramafic intrusion, western
Sulfur contents at sulfide-liquid or anhydrite saturation in silicate melts: Empirical equations and
Abundant Fe–Ti oxide inclusions in olivine from the Panzhihua and Hongge layered intrusions, SW Chin
Controls on the Fo and Ni contents of olivine in sulfide-bearing mafic-ultramafic intrusions: Princi
Applications of stable and radiogenic isotopes to magmatic Cu-Ni-PGE deposits: Examples and cautions
Cr-spinel/melt and Cr-spinel/olivine nickel partition coefficients from basalts, picrites and intrus
Origin of the inconsistent apparent Re–Os ages of the Jinchuan Ni–Cu sulfide ore deposit, China : Po
Textural and stable isotope studies of hydrothermal alteration in the Main Sulfide Zone of the Great
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