| 金平多衣梁钨多金属矿床地质特征及找矿方向 |
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| 引用本文： | 张苗红,杨开军,徐恒.金平多衣梁钨多金属矿床地质特征及找矿方向[J].四川地质学报,2010,30(4):424-426. |
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| 作者姓名： | 张苗红 杨开军 徐恒 |
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| 作者单位： | 云南省有色地质局地质地球物理化学勘查院,昆明650216 |
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| 摘 要： | 金平多衣梁钨多金属矿床大地构造位置处于青藏滇板块与扬子板块的交接拼合部位,挟持于北西向的阿墨江断裂和哀牢山深大断裂之间2的南东边缘。通过对矿床区域地质背景、矿床地质特征、控矿因素及矿床成因等初步研究,综合地质成矿信息总结出了找矿标志,并以此提出了有利找矿方向。
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| 关 键 词： | 钨多金属矿床 地质特征 找矿方向 云南金平 |
Geological Features and Range of Reconnaissance for the Duoyiliang W-polymetallic Deposit in Jinping, Yunnan |
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| ZHANG Miao-hong,YANG Kai-jun,XU Heng.Geological Features and Range of Reconnaissance for the Duoyiliang W-polymetallic Deposit in Jinping, Yunnan[J].Acta Geologica Sichuan,2010,30(4):424-426. |
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| Authors: | ZHANG Miao-hong YANG Kai-jun XU Heng |
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| Institution: | (Institute of Geophysical and Geochemical Exploration,Yunnan Bureau of Geology of Nonferrous Metals,Kunming 650216) |
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| Abstract: | The Duoyiliang W-polymetallic deposit in Jinping,Yunnan lies between the Amojiang fault and the Ailaoshan fault in the plate junction between the Qinghai-Tibet-Yunnan plate and The Yangtze plate.This paper deals with regional geological setting,geological features,ore control factors and genesis for the deposit and accordingly makes an approach to its range of reconnaissance. |
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| Keywords: | W-polymetallic deposit geological feature range of reconnaissance Jinping Yunnan |
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