| 湖北黄梅菱铁矿矿床成矿作用的古水文地质学研究 |
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| 引用本文： | 王焰新
,沈照理.湖北黄梅菱铁矿矿床成矿作用的古水文地质学研究[J].现代地质,1988,2(1):110. |
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| 作者姓名： | 王焰新 沈照理 |
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| 摘 要： | 本文从古水文地质角度探讨了黄梅菱铁矿矿床的成矿机制,结果证实,古水文地质学研究无论对矿床学,还是对水文地质学,都可以提供一些新的信息和认识。作者的研究表明,黄梅菱铁矿矿床是含矿岩系（石炭系黄龙组和二叠系栖霞组碳酸盐岩）沉积期后变化与印支运动共同作用的产物;以沉积水为主,后期的混合水为次的地下水,构成了该矿床的成矿溶液。
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| 关 键 词： | 菱铁矿 成矿溶液 水文地质 |
A PALEOHYDROGEOLOGICAL STUDY ON THE GENESIS OF THE HUANGMEI (HUBEI,CHINA) SIDERITE ORE DEPOSIT |
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| Wang Yanxin Shen Zhaoli.A PALEOHYDROGEOLOGICAL STUDY ON THE GENESIS OF THE HUANGMEI (HUBEI,CHINA) SIDERITE ORE DEPOSIT[J].Geoscience——Journal of Graduate School,China University of Geosciences,1988,2(1):110. |
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| Authors: | Wang Yanxin Shen Zhaoli |
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| Institution: | China University of Geosciences |
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| Abstract: | The ore genesis of the famous Huangmei siderite ore deposit is discussed from the viewpoints of paleohydrogeology. It is proved that such kind of researches can provide insights both into ore geology and hydrogeology. The results show that the siderite is the product of postdepositional changes of the Permian-Carboniferous carbonate hostrocks with the co-working of the Indo-Chinese tectonic movement, while the ore-forming fluid is the groundwater mainly of sedimentary origin. |
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| Keywords: | : Siderite Ore-forming solution Hydrogeology |
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