江西上饶县上村钒多金属矿床地质特征及找矿方向

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英文篇名：Geological characteristics and prospecting direction of the Shangcun vanadium polymetallic deposit in Shangrao county, Jiangxi province 作者：周丁根 ; 周先军 ; 王平 ; 胡振 英文作者：ZHOU Dinggen;ZHOU Xianjun;WANG Ping;HU Zhen;The First Geological Team of Jiangxi Nonferrous Metals Geological Exploration Bureau; 关键词：矿床地质 ; 钒多金属矿 ; 石煤型钒矿 ; 矿床成因 ; 找矿方向 英文关键词：mineral geology;;vanadium polymetallic deposit;;stone-coal type vanadium ore;;deposits genesis;;prospecting direction 中文刊名：SHAD 英文刊名：Shanghai Land & Resources 机构：江西有色地质勘查一队; 出版日期：2019-03-30 出版单位：上海国土资源 年：2019 期：v.40 基金：中国地质调查局地质调查项目;; 江西省地质勘查基金项目“江西省上饶县上村钼钒多金属矿调查评价”(2012-39) 语种：中文; 页：SHAD201901021 页数：5 CN：01 ISSN：31-2062/P 分类号：105-109

摘要

上饶上村钒多金属矿赋存于寒武系荷塘组底部石煤层中,受地层、岩性、岩相古地理及古构造条件控制。矿石类型有含钒石煤矿石,含钒硅质岩矿石,含钒炭(硅)质板岩矿石等,主要含钒矿物为含钒水云母。钒的成矿与成岩是同时进行的,同时叠加了生物地球化学成矿作用和海底热水喷流成矿作用。矿床成因类型可归为海相生物和生物地球化学作用形成,并有喷流热水参与的同生沉积矿床。通过对上村钒多金属矿床地质特征、矿床成因及找矿标志的总结分析,指出了江西寻找石煤型钒矿的方向。
        The Shangcun vanadium polymetallic deposit in Shangrao County is derived from the underlying stone-coal layer of the Cambrian Hetang Formation and is controlled by strata, lithology, lithofacies, paleogeography and paleostructural conditions. The ore types include vanadium-bearing stone-coal ore, vanadium-bearing silicalite ore and vanadium-bearing carbon(silicon) slate ore. The main vanadium-bearing mineral is vanadium-bearing hydromica. The metallogenic and diagenetic processes of vanadium are simultaneous as is the superimposition of biogeochemical mineralization and seabed hot-water jet metallogenesis. The genetic types of the deposits can be divided into syngenetic sedimentary deposits formed by the mineralization of marine organism and biogeochemistry with jet hot waterThis paper summarizes and analyzes the geological characteristics, genesis and ore-prospecting criteria of the Shangcun vanadium polymetallic deposit in Shangrao County and indicates the direction forfinding vanadium deposits in the stone-coal type in Jiangxi province.

引文

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