内蒙古毛盖吐铜钼矿床地质特征
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摘要
本文在前人地质资料的基础上,对内蒙古毛盖吐铜钼矿床进行了地质特征研究。通过矿床区域上成矿地质背景、矿床地质特征、矿体特征等的总结和研究,初步确定矿床的空间分布规律、控矿条件及成矿规律。在此基础之上又研究了矿区花岗闪长岩的岩石地球化学特征,进一步确定了矿床形成时所处的岩浆-构造环境。又利用矿石中的原生流体包裹体,测定和计算了矿床成矿物理化学条件。最后综合讨论了毛盖吐矿床的成矿流体性质、成矿地质条件、地球化学特征、成矿时代和成矿类型。
Maogaitu Copper-molybdenum Deposit is located in the metallogenic belt of southern GreaterHiggnanmountains.It is a new-found deposit that is of low study.
Maogaitu Copper-molybdenum Deposit is focused on the Yanshanian granodio -rite,which putting up local mineralizing in this rock. The mineral veins and ore bodies is controlled by the fractures which are west-eastern in the mining site and distributed with right diagonal.Mineralization body alteration belts have been founded.and one of them has been checked by projects that there are 12 copper-molybdenum ore bodies in it.Copper-molybdenum ores major in the mineralized K-feldspar - quartz belt, granite- quartz belt.
Showing the results of petrochemistry microelement geochemistry, the granodiorite which has genesis relationship with the deposit is of calc-alkalineseries.It belongs to M-type granite that is formed in island-arc circumstance which is between the ocean and the continent.
Fluid inclusions research indicates that the deposit from the gas-liquid fluid inclusions composed of two-phase inclusions. The homogenization temperature is 178.9~236.1℃.The peak value is 170~200℃and 210~240℃.Liquid inclusions solinty is 1.05~40.8wt%(NaCl).The density is 0.82~0.89g/cm3.The estimating matallogentic pressure is 14.00~18.00MPa.The depth is 0.50~0.65km.
To sum up,the formation of Maogaitu copper-molybdenum deposit relate to the subduction of Pacific Plate to the the Eurasian Plate.The hanging side of the Subduction zone is a extending circumstance of . island-arc or back-arc。In addition,the E-W Huolinghe River faulted zone coincides with the NNE Hundule River faulted zone in the granodiorite rock. Therefore the copper-molybdenum deposit of shallow-seated middle-low temperature hydrothermal origin is formed that relate to the granodiorite.
Maogaitu Copper-molybdenum Deposit is located in the metallogenic belt of southern GreaterHiggnanmountains.It is a new-found deposit that is of low study.
Maogaitu Copper-molybdenum Deposit is focused on the Yanshanian granodio -rite,which putting up local mineralizing in this rock. The mineral veins and ore bodies is controlled by the fractures which are west-eastern in the mining site and distributed with right diagonal.Mineralization body alteration belts have been founded.and one of them has been checked by projects that there are 12 copper-molybdenum ore bodies in it.Copper-molybdenum ores major in the mineralized K-feldspar - quartz belt, granite- quartz belt.
Showing the results of petrochemistry microelement geochemistry, the granodiorite which has genesis relationship with the deposit is of calc-alkalineseries.It belongs to M-type granite that is formed in island-arc circumstance which is between the ocean and the continent.
Fluid inclusions research indicates that the deposit from the gas-liquid fluid inclusions composed of two-phase inclusions. The homogenization temperature is 178.9~236.1℃.The peak value is 170~200℃and 210~240℃.Liquid inclusions solinty is 1.05~40.8wt%(NaCl).The density is 0.82~0.89g/cm3.The estimating matallogentic pressure is 14.00~18.00MPa.The depth is 0.50~0.65km.
To sum up,the formation of Maogaitu copper-molybdenum deposit relate to the subduction of Pacific Plate to the the Eurasian Plate.The hanging side of the Subduction zone is a extending circumstance of . island-arc or back-arc。In addition,the E-W Huolinghe River faulted zone coincides with the NNE Hundule River faulted zone in the granodiorite rock. Therefore the copper-molybdenum deposit of shallow-seated middle-low temperature hydrothermal origin is formed that relate to the granodiorite.
引文
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