| 阿沙勒金矿地质特征及成因初探 |
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| 引用本文： | 杨泽军,靖军,郭德红.阿沙勒金矿地质特征及成因初探[J].新疆地质,1999(3). |
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| 作者姓名： | 杨泽军 靖军 郭德红 |
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| 作者单位： | 武装警察部队黄金第十五支队!新疆乌鲁木齐830057 |
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| 基金项目： | 武警黄金指挥部 HJ97-2 -2科研项目 |
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| 摘 要： | 阿沙勒金矿产于华力西早期花岗闪长岩与上奥陶统呼独克达坂组外接触带泥质灰岩、砂砾岩中,受断裂破碎带控制,矿体呈舒缓波状,具膨大收缩特征。矿体地表及浅部为氧化矿,矿石类型为破碎蚀变岩型。成矿物质来源与赋矿地层及花岗闪长岩有关,属夕卡岩型金矿床
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| 关 键 词： | 阿沙勒金矿 地质特征 物质来源 矿床成因 |
PRELIMINARY DISCUSSION ON THE GENESIS AND GEOLOGI CAL CHARACTERISTICS OF ASHALE GOLD DEPOSIT |
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| YANG Ze jun,JING Jun,GUO De hong.PRELIMINARY DISCUSSION ON THE GENESIS AND GEOLOGI CAL CHARACTERISTICS OF ASHALE GOLD DEPOSIT[J].Xinjiang Geology,1999(3). |
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| Authors: | YANG Ze jun JING Jun GUO De hong |
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| Abstract: | The Ashale gold deposit is produced in the argillaceous limestone and sand conglomarate of Hudukedaban Formation of Upper Ordovician,which belongs to the external contacting belt of Early Variscan granodiorite.It is controlled by the fault belt.It waves weekly and is widden or narrowed partly.There is an orogenic belt on the ground and in the lower part.The source rock of metallogy and hosting rock are related to the granodiorite.It belongs to a skarn gold deposit. |
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| Keywords: | Ashale gold deposit geological characteristics material sources genesis of ore deposit |
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