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 |
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Main Authors | , , , |
Format | Journal Article |
Language | Chinese |
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 |
Subjects | |
Online Access | Get full text |
ISSN | 2095-1329 |
DOI | 10.3969/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。 |
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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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