摘要
江西临川市荣山Ｊ３—Ｔ３盆地与基底变质岩之间的滑覆构造，以地层减薄、缺失和产状变陡为特征。本文在分析滑覆构造特点的基础上，探讨了其成因机制，进而分析了滑覆构造与该区金矿化之间的关系，并作了富金矿可能存在部位的初步预测。
Gliding nappe tectonics of rongshan is located between J_3 T_3 basin and basement metamorphic rocks. Its features are stratigraphic thin or break and attitude became steeper. This paper analysed these features,their formation mechanism and its relation to gold mineralization.Finally the prognostication of high grade gold deposit location is made
出处
《华东地质学院学报》
1996年第4期374-377,共4页
Journal of East China Geological Institute
关键词
逆冲断层
滑覆构造
金矿床
矿化
thrust fault
gliding nappe
gold mineralization
