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初论成矿流体及金属矿物富集系统
引用本文:芮宗瑶,李荫清,王龙生,王义天.初论成矿流体及金属矿物富集系统[J].矿床地质,2002,21(1):83-90.
作者姓名:芮宗瑶  李荫清  王龙生  王义天
作者单位:中国地质科学院矿产资源研究所,北京,100037
摘    要:在长期积累的有关金属成矿作用的研究资料和成果的基础上,吸收和借鉴相关学科领域的最新研究进展,作者初步提出了一个新的金属成矿系统分类方案。本篇首先介绍10种成矿流体及其金属矿物富集系统的主要特征,10种系统包括:镁铁质岩浆中的堆积系统、镁铁质岩浆与硫化物熔融体不混溶系统、长英质岩浆与挥发相不混溶系统、热水中矿物子相析出系统、热水与CO2不混溶系统、热水与有机物不混溶系统、变质热水矿物子相析出系统、地下水矿物子相析出系统、地表水中的堆积系统和地表水中矿物子相溶解系统。

关 键 词:成矿流体  成矿系列  矿物子相析出  矿物子相溶解  金属矿物  岩浆  硫化物
文章编号:0258-7106(2002)01-0083-07

Preliminary Discussion on Oreforming Fluids and Enrichment Systems of Metallic Mnerals
Rui Zongyao,Li Yinqing,Wang Longsheng,Wang Yitian.Preliminary Discussion on Oreforming Fluids and Enrichment Systems of Metallic Mnerals[J].Mineral Deposits,2002,21(1):83-90.
Authors:Rui Zongyao  Li Yinqing  Wang Longsheng  Wang Yitian
Abstract:On the basis of the data accumulated and the achievements made by the authors concerning the metallic mineralization during their long period of research work, combined with a reference of the new advances in related research fields, they have preliminarily formulated a new systematic scheme for the metallogenic system, and are planning to write a series of papers to deal in detail with the new scheme. In this paper, ten sorts of ore-forming fluids and enrichment systems of metallic minerals as well as their features are presented for the first time. These systems include the accumulation system in mafic magma, the immiscible system of mafic magma and sulfide molten mass, the immiscible system of felsic magma and volatile phase, the separation system of mineral sub-phase in hydrothermal solution, the immiscible system of hydrothermal solution and CO 2, the immiscible system of hydrothermal solution and organic material, the separation system of mineral sub-phase in metamorphic hydrothermal solution, the separation system of mineral sub-phase in groundwater, the accumulation system in surface water, and the solution system of mineral sub-phase in surface water.
Keywords:ore-forming fluids  metallogenic series  separation of mineral sub-phase  solution of mineral sub-phase
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