云南个旧南部含矿断裂带与成矿元素空间展布特征——以龙树脚断裂为例  

SPATIAL DISTRIBUTION CHARACTERISTICS OF MINERALIZED FRACTURE ZONE AND METALLOGENETIC ELEMENTS IN THE SOUTH OF GEJIU ORE DISTRICT, YUNNAN PROVINCE--Take Longshujiao fault as an example

作　　者：高建国[1] 念红良[1] 陈仕炎[1] 李西[1] 郭君[1] 

机构地区：[1]昆明理工大学地球科学系,昆明650093

出　　处：《地质找矿论丛》2004年第4期238-242,共5页Contributions to Geology and Mineral Resources Research

基　　金：云南省省校省院科技合作项目(项目编号:2000YK 05)资助。

摘　　要：　文章以龙树脚断裂为例,系统分析了个旧南部地区含矿断裂带的空间展布特征以及矿体和成矿元素在断裂带中的分布特征。提出在含矿断裂带走向和倾向的波状起伏部位、含矿元素分布向深部延伸的部位仍有较大的找矿空间。The paper takes Longshujiao fault zone as an example, analyzes systematically characteristics of distribution of ore host fault and orebody and metallogenetic element in the south of Gejiu ore district, It presents that there is still larger ore-searching space in the wavy position of the host fault in the strike and dip directions, and the position at which metallogenetic element contour extend to depth.

关 键 词：含矿断裂 成矿元素 个旧南部地区 云南省 

分 类 号：P613[天文地球—矿床学] P618.44[天文地球—地质学]