摘要
从分析川滇黔相邻区铅锌矿床分布特征着手,以成矿元素继承演化为主线,阐述了该区从最初铅锌地球化学块体形成,到古生代受岩相古地理控制的元素演化、成矿期元素活化、流体成矿,最后造山期叠加改造成矿的规律。
This paper deals with protogenetic Pb-Zn geochemical blocksl Paleozoic evolution controlled by sedimentary facies and paleogeography, mobilization and ore-formation in mineralized phase and late reformation in the Sichuan-Guizhou-Yunnan border region based on distribution of the Pb-Zn Deposits.
出处
《四川地质学报》
2012年第3期304-308,共5页
Acta Geologica Sichuan
关键词
铅锌矿床
分布特征
成矿规律
川滇黔相邻区
Pb-Zn Deposit
distribution
metallogeny
Sichuan-Guizhou-Yunnan border region
