| 青海省冷湖小赛什腾铜矿岩屑地球化学特征 |
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| 引用本文： | 丁兆举,袁涛,王平户.青海省冷湖小赛什腾铜矿岩屑地球化学特征[J].地质找矿论丛,2005,20(Z1):190-193. |
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| 作者姓名： | 丁兆举 袁涛 王平户 |
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| 作者单位： | 中国冶金地质勘查工程总局,西北地质勘查院,西安,710061 |
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| 摘 要： | 文章总结了小赛什腾铜矿的地球化学特征,认为闪长岩体本身含铜,岩体内存在着多期多阶段矿化叠加及多种矿化类型,平面上元素分带明显.指出了Cu,Au,Mo异常叠合部位仍是重点找矿地段.
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| 关 键 词： | 小赛什腾铜矿 岩屑地球化学特征 青海省 |
| 文章编号： | 1001-1412(2005)S0-0190-04 |
| 修稿时间： | 2005年4月5日 |
GEOCHEMICAL CHARACTERISTICS OF XIAOSERTENG COPPER CAMP IN LENGHU, QINGHAI PROVINCE |
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| DING Zhao-ju,YUAN Tao,WANG Ping-hu.GEOCHEMICAL CHARACTERISTICS OF XIAOSERTENG COPPER CAMP IN LENGHU, QINGHAI PROVINCE[J].Contributions to Geology and Mineral Resources Research,2005,20(Z1):190-193. |
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| Authors: | DING Zhao-ju YUAN Tao WANG Ping-hu |
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| Abstract: | The paper summarizes the geochemical charateristics of Xiaoserteng Cu camp. Diorite is the Cu-bearing rock and multi-stage and several ore-forming epches took place in the diorite body and they are supimposed thus different mineralizations and ores occur. In plane elements are zoned. Overprint of Cu, Au, Mo is favorable for ore formation. |
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| Keywords: | Xiaoserteng copper camp geochemical characteristics Qinghai province |
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