江西上饶县上村钒多金属矿床地质特征及找矿方向

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。...

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Published in上海国土资源 Vol. 40; no. 1; pp. 101 - 105
Main Authors 周丁根, 周先军, 王平, 胡振
Format Journal Article
LanguageChinese
Published 上海市地质学会 01.03.2019
上海市地质调查研究院
江西有色地质勘查一队,江西·鹰潭 335003
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ISSN2095-1329
DOI10.3969/j.issn.2095-1329.2019.01.021

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Abstract 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。
AbstractList P618.61; 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.
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。
Author 胡振
周先军
周丁根
王平
AuthorAffiliation 江西有色地质勘查一队,江西·鹰潭 335003
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WANG Ping
ZHOU Xianjun
ZHOU Dinggen
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Keywords 矿床成因
矿床地质
石煤型钒矿
钒多金属矿
找矿方向
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P618.61; 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,...
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Title 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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