黔东成矿带铅锌成矿作用刍议
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摘要
铅锌属于紧缺资源之一,"湘西—黔东铅锌成矿带"是我国重要铅锌成矿带之一,贵州境内部分称为"黔东成矿带",该区铅锌矿床(点)分布广泛,具有成群成带分布等特征。由于相关地质地球化学研究相对薄弱,黔东地区铅锌地质勘探进展缓慢,并未像湘西地区一样取得重大突破。本文通过总结"黔东成矿带"内铅锌成矿作用地质与地球化学特征,探讨该区存在的诸多科学研究薄弱环节,结合MVT铅锌矿床研究现状,提出该区铅锌成矿作用与MVT矿床基本一致,是国内研究MVT铅锌矿床理想基地,采用原位分析等先进测试技术,加强矿床地质地球化学特征对比、成矿物质来源、成矿流体和同位素定年等研究,以揭示各矿区与区域成矿流体系统的性质及其演化,建立合理成矿模式及与研究区构造和古油藏演化的关系,并探讨其形成的动力学背景,不仅突出黔东MVT铅锌成矿作用特色,从而促进MVT铅锌矿成矿作用和分散元素超常富集理论发展,更重要的是可为拓宽黔东地区铅锌找矿思路提供理论依据。
Lead and zinc mineral resources are among mostly short resources in China. The "Xiangxi-Qiandong Pb-Zn metallogenic belt" is an important Pb-Zn belt in China. Its part in Guizhou Province is called the "Qiandong metallogenic belt" in which Pb-Zn deposits(mineral occurrences) are widely distributed in clusters and zones. Due to limited researches on relevant geology and geochemistry, the Pb-Zn geological exploration in the Qiandong district is far away to the great success of the Pb-Zn exploration in the Xiangxi district. In the paper, we have summarized geological and geochemical characteristics of the Pb-Zn mineralization in the "Qiandong metallogenic belt" and discussed deficiencies of scientific researches on the Pb-Zn mineralization in this district. Combined with the research actualities of MVT Pb-Zn deposits, it is proposed that characteristics of the Pb-Zn mineralization in the Qiandong district are in accordance with those of MVT deposits, and the Qiandong district is an ideal area for studying MVT deposits in China. Moreover, the in-situ analytical techniques are applied to strengthen the comparison of geological and geochemical characteristics of the deposits, the studies of ore-forming material sources, ore-forming fluid sources, and isotopic dating, in order to reveal the nature and evolution of ore-forming fluids systems in each deposit and in the district, to establish a reasonable metallogenic model, to clarify the relationship between the regional structure and the evolution of fossil oil reservoir, and to discuss the geodynamic background of the Pb-Zn metallogeny in the Qiandong metallogenic belt. This study has not only highlighted the features of the MVT Pb-Zn mineralization in the Qiandong district, thus to promote the development of theories regarding to the MVT Pb-Zn mineralization and the super-enrichment of disperse elements, but also has provided fundamental theoretical basis for widening the thought of the Pb-Zn prospecting in the Qiandong district.
Lead and zinc mineral resources are among mostly short resources in China. The "Xiangxi-Qiandong Pb-Zn metallogenic belt" is an important Pb-Zn belt in China. Its part in Guizhou Province is called the "Qiandong metallogenic belt" in which Pb-Zn deposits(mineral occurrences) are widely distributed in clusters and zones. Due to limited researches on relevant geology and geochemistry, the Pb-Zn geological exploration in the Qiandong district is far away to the great success of the Pb-Zn exploration in the Xiangxi district. In the paper, we have summarized geological and geochemical characteristics of the Pb-Zn mineralization in the "Qiandong metallogenic belt" and discussed deficiencies of scientific researches on the Pb-Zn mineralization in this district. Combined with the research actualities of MVT Pb-Zn deposits, it is proposed that characteristics of the Pb-Zn mineralization in the Qiandong district are in accordance with those of MVT deposits, and the Qiandong district is an ideal area for studying MVT deposits in China. Moreover, the in-situ analytical techniques are applied to strengthen the comparison of geological and geochemical characteristics of the deposits, the studies of ore-forming material sources, ore-forming fluid sources, and isotopic dating, in order to reveal the nature and evolution of ore-forming fluids systems in each deposit and in the district, to establish a reasonable metallogenic model, to clarify the relationship between the regional structure and the evolution of fossil oil reservoir, and to discuss the geodynamic background of the Pb-Zn metallogeny in the Qiandong metallogenic belt. This study has not only highlighted the features of the MVT Pb-Zn mineralization in the Qiandong district, thus to promote the development of theories regarding to the MVT Pb-Zn mineralization and the super-enrichment of disperse elements, but also has provided fundamental theoretical basis for widening the thought of the Pb-Zn prospecting in the Qiandong district.
引文
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