| 西藏俄卡地银多金属异常区地球化学 |
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| 引用本文： | 王铨宇,杨树元.西藏俄卡地银多金属异常区地球化学[J].云南地质,2005,24(3):298-302. |
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| 作者姓名： | 王铨宇 杨树元 |
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| 作者单位： | 云南省地质调查院物化探所,昆明,宜良,652100 |
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| 摘 要： | 异常形态、分布严格受推覆断裂控制,范围大、浓集中心明显,浓度变化及因子载荷表明。区内找Ag、Pb有利,而Sb又为其最佳指示元素。
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| 关 键 词： | 地球化学异常 推覆断裂控制 银铅成矿有利 俄卡地西藏 |
| 文章编号： | 1004-1885（2005）03-298-05 |
| 收稿时间： | 2005-04-11 |
| 修稿时间： | 2005-04-11 |
ON THE GEOCHEMISTRY OF EKADI AG POLYMETALLIC ANOMALY AREA, XIZANG |
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| WANG Quan-yu.ON THE GEOCHEMISTRY OF EKADI AG POLYMETALLIC ANOMALY AREA, XIZANG[J].Yunnan Geology,2005,24(3):298-302. |
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| Authors: | WANG Quan-yu |
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| Abstract: | The morphology and distribution of anomaly are strictly controlled by the nappe fault, which is characterized by a large distribution range, an evident concentration centre and the evident change of concentration. The factor loading shows that this area is advantageous to the prospecting for Ag, Pb, and Sb is the best indicator element. |
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| Keywords: | Geochemical Anomaly Nappe Fault Controlling Advanta geous to Prospecting for Ag Pb Ekadi Xizang |
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