摘要
赣西卡林型金矿床各类岩矿石的稀土元素地球化学特征的研究表明，与卡林型金矿成矿有关的岩浆岩，其成因是过渡型地壳同熔型成因系列。成矿物质源于容矿围岩及基底地层，部分成矿物质源于下二叠统茅口组，属海底喷流沉积成因。
Based on the study of REE geochemical features about various types of host rocks in Carlin type gold deposits of western Jiangxi, it shows that the genesis of magmatites associated with the mineralization of Carlin type gold deposits pertains to that of crustal syntectic type series, the metallogenic materials originate mainly from host rocks and basement strata, partly from Maokou formation of lower Permian, Such types of deposits are of submarine spout-sedimentary deposits.
出处
《矿产与地质》
1998年第5期335-341,共7页
Mineral Resources and Geology
