摘要
系统的常量元素、微量元素和稀土元素地球化学分析表明，皖南下震旦统雷公坞组碎屑岩，属弧后盆地沉积。以井潭组为代表的岛弧钙碱性火山岩区是其物源区。
A detailed geochemical analysis of major,trace and rare earth elements suggests that clastic rocks of Leigongwu Formation,Lower Sinian in southern Anhui derived from calc-alkaline volcanic are represented by JingtanFormation and deposited in a backarc basin.
出处
《安徽地质》
1996年第4期15-22,共8页
Geology of Anhui
基金
中国有色金属工业总公司"八五"银矿基金
关键词
地球化学
物源区
沉积大地构造背景
雷公坞组
皖南
geochemistry
provenance
sedimentary tectonic
Leigongwu Formation
southern Anhui
