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-改造层控型矿床。
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.
出处
《矿产与地质》
2008年第4期293-296,共4页
Mineral Resources and Geology
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
Pb-Zn-Cu polymetallic deposit, geologic characteristics,genesis discussion, prospecting indicators, Lanping County
