摘要
昆阳裂谷(云南段)是重要的铁铜矿化集中区,伴随裂谷的发展演化过程,铁铜矿床的成矿具有"六楼一梯"的时空分布规律,区内成矿主要受地层层位、岩相及古地理环境、构造以及火山作用等因素的控制,根据区域成矿规律特征,总结出区内4个重点找矿靶区及重要找矿地段.
The Kunyang rift mineralization belt is one of the most significant iron and copper metallogenetic belts in Yunnan,whose deposits share a common temporal and spatial regularity, the ＂six stories with one ladder＂. The iron and copper poly - metallic mineralization in this area is mainly controlled by the strata, lithofacies, paleogeo- graphical environment, structures and the volcanism. Four major exploration targets and some specific section with high potential for iron and copper deposits are then made clear for further exploration.
出处
《昆明理工大学学报（理工版）》
北大核心
2009年第5期5-9,17,共6页
Journal of Kunming University of Science and Technology(Natural Science Edition)
基金
云南省国际合作项目(项目编号:2002GH11)
关键词
铁铜矿床
成矿规律
成矿预测
昆阳裂谷
云南
iron and copper deposit
metallogenesis
metallogenetic prediction
Kunyang rift
Yunnan
