摘要
本文通过硫、氢、氧、碳、铅同位素组成的研究，认为成矿溶液来自大气降水，成矿物质来自南羊山组和袁家沟组的不纯细碎屑岩—碳酸盐岩。在此基础上分析了成矿过程。
This paper presents S, H, O, C isotopic data obtained from Qiuling micro-fine disseminated gold deposit. H2O in.ore fluid is mainly from ancient meteoric water. Ore-forming materials are dominated by those derived from impure-fine clasitic carbonate rock of Nanyangshan Formation and Yuanjiagou Formation. Then ore-forming processes are analysed.
出处
《地质找矿论丛》
CAS
CSCD
1996年第4期27-34,共8页
Contributions to Geology and Mineral Resources Research
