| 云南省兰坪县凤岩山铅锌铜多金属矿地质特征及成因探讨 |
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| 引用本文： | 武龙祥,刘江波,张准,杨吉忠.云南省兰坪县凤岩山铅锌铜多金属矿地质特征及成因探讨[J].矿产与地质,2008,22(4):293-296. |
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| 作者姓名： | 武龙祥 刘江波 张准 杨吉忠 |
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| 作者单位： | 1. 云南有色地质局,楚雄勘察院,云南,楚雄,675000
2. 云南国土资源职业学院,云南,昆明,650217 |
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| 摘 要： | 凤岩山铅锌铜多金属矿位于兰坪断陷盆地中部，具有良好的成矿条件和找矿前景。文章通过对矿区地质背景条件、地质特征、地球化学异常特征、矿体特征、矿石特征的分析，推断矿床成因为后期热卤水为主改造叠加形成，属沉积一改造层控型矿床。
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| 关 键 词： | 铅锌铜多金属矿床 地质特征 成因探讨 找矿标志 兰坪县 |
Geological characteristics and genesis discussion of the Fengyanshan Pb-Zn-Cu polymetallic deposit, Lanping County of Yunnan Province |
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| WU Long-xiang,LIU Jiang-bo,ZHANG Zhun,YANG Ji-zhong.Geological characteristics and genesis discussion of the Fengyanshan Pb-Zn-Cu polymetallic deposit, Lanping County of Yunnan Province[J].Mineral Resources and Geology,2008,22(4):293-296. |
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| Authors: | WU Long-xiang LIU Jiang-bo ZHANG Zhun YANG Ji-zhong |
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| Institution: | WU Long-xiang, LIU Jiang-bo, ZHANG Zhun, YANG Ji-zhong (1. Chuxiong Reconnaissance Institute of Yunnan Non-ferrous Metal Geology Bureau, Chuxiong, Yunnan 675000, China; 2. Yunnan Land Resources Professional College, Kunming 650217, China) |
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| Abstract: | The Fengyanshan Pb-Zn-Cu polymetallic deposit located in central area of the Lanping fault basin and has a well ore-forming conditions and prospecting perspective. It has concluded that the deposit was formed mainly by alteration and superposition of later hot brine and belongs to sedimentary-alteration stratabound deposit through analyzing the geological background, geological characteristics, geochemical anomalies＇ characteristics, orebodies＇ characteristics, ores＇ characteristics of the ore area. |
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| Keywords: | Pb-Zn-Cu polymetallic deposit geologic characteristics genesis discussion prospecting indicators Lanping County |
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