| 东昆仑开荒北金矿床地质特征及控矿条件 |
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| 引用本文： | 闫臻,胡正国,刘继庆,李厚民,钱壮志,孙继东.东昆仑开荒北金矿床地质特征及控矿条件[J].地球科学与环境学报,2000,22(1). |
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| 作者姓名： | 闫臻 胡正国 刘继庆 李厚民 钱壮志 孙继东 |
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| 作者单位： | 西安工程学院,资源与材料工程系,陕西,西安,710054 |
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| 基金项目： | 原地矿部 (地科定 95 18)项目 |
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| 摘 要： | 开荒北金矿床是东昆仑昆南带颇具代表性的金矿床 ,笔者通过研究后认为 ,中三叠统闹仓坚沟组为该矿床的矿源层 ,隐伏岩体 (?)为成矿提供热源 ,经过晚期的动力作用改造 ,成矿物质进一步富集 ,矿体规模加大 ,矿床具层控改造的特征
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| 关 键 词： | 开荒北金矿床 昆南带 矿源层 层控改造 新疆 |
GEOLOGICAL CHARACTERISTICS AND CRE-CONTROL FACTORS OF KAIHUANGBEI GOLD DEPOIST IN EASTY KUNLUN MOUNTAIN |
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| YAN Zhen,HU Zheng-guo,LIU Ji-qing,LI Hou-min,QIAN Zhuang-zhi,SUN Ji-dong.GEOLOGICAL CHARACTERISTICS AND CRE-CONTROL FACTORS OF KAIHUANGBEI GOLD DEPOIST IN EASTY KUNLUN MOUNTAIN[J].Journal of Earth Sciences and Environment,2000,22(1). |
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| Authors: | YAN Zhen HU Zheng-guo LIU Ji-qing LI Hou-min QIAN Zhuang-zhi SUN Ji-dong |
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| Abstract: | Kaihungbei gold depoist is a represtntative one of the south belt in the east KunLun mountain after studying, it is suggested that Naocangjiangou formation(T 2) is source bed, buried rock mass(?) provides heat resource for metallogenic process The dynamical reformation made mineralizing resource enrich again, the scale of ore body expanded in late period. Stratabound refourmation is the typical characters of the depoist After analyszing the above ,it is guided to search for the same typical gold depoist in south belt of Kunlun mountain |
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| Keywords: | Kaihuangbei gold depoist south belt of Kunlun mountain strataboundreformation |
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