| 内蒙古甲生盘铅锌硫矿床成因探讨 |
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| 引用本文： | 张玉清.内蒙古甲生盘铅锌硫矿床成因探讨[J].内蒙古地质,1998(3). |
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| 作者姓名： | 张玉清 |
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| 作者单位： | 内蒙古第一区域地质研究院 |
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| 摘 要： | 甲生盘铅锌硫矿床是一个大型层控矿床，赋存于中元古界渣尔泰山群阿古鲁沟组白云质灰岩、砂质白云岩之中，属海底火山喷气—沉积成因。该碳酸盐岩为一套滨海—浅海碳酸盐台地相沉积，同生滑动现象十分发育，存在着古同生断裂，为火山喷气提供了通道。台地坡底沟相这一独特的环境，又为成矿物质的富集提供良好的场所。
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| 关 键 词： | 甲生盘 铅锌硫 火山喷气-沉积 矿床成因 |
A Discuss Genesis of Jiashengpan Lead, Zinc and Sulphur Deposit in Inner Mongolia |
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| Zhang,Yuqing.A Discuss Genesis of Jiashengpan Lead, Zinc and Sulphur Deposit in Inner Mongolia[J].Geology of Inner Mongolia,1998(3). |
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| Authors: | Zhang Yuqing |
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| Institution: | The First Regional Geological Institute of Inner Mongolia |
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| Abstract: | Jiashengpan lead,zinc and sulphur deposit is a large stratabound deposit which is occurred in dolomitic limestone,sandy dolomite of Agulugou formation of Chaertaishan group of middle proterozoic Earthen.The deposit belongs to submarine volcanic exhalation-sedimentary genesis.The carbonate rock is a suite of littoral-shallow sea carbonate platform facial sediment,contemporaneous sliding was very development.It exists in palaeocontemporaneous fault and supply channels for volcanic exhalation.The platform slope bottom facies that a well position to supply the sandy material of rich is a specially environment. |
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| Keywords: | Jiashengpan lead-zinc sulphur volcanic exhalation-sediment mineralization genesis |
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