摘要
介绍粤西连州氧化型铁锰矿矿床地质、矿石特征,分析矿床的成矿机制。认为该矿床具备热液矿床、次生矿床双重特征,燕山期前就位连州断裂的原生多金属矿带,后期受古地形、气候因素作用,形成现有的氧化型铁锰矿。
This paper deal with the geological features,Ore characteristics,and minerogenic mechanism of lianzhou Fe-AAn deposit in the west of Guangdong Province.This deposit has hydrothermal deposit,secondary deposit dual characteristics,fracture structure,before Yanshan period the deposit is primary polymetallic ore belt in lianzhou fracture structure,Late by ancient terrain,climate factors,form the existing type iron manganese oxide.
出处
《西部资源》
2016年第1期21-24,共4页
Western Resources
基金
广东省财政地质专项经费项目(粤财工[2010]518号)资助成果
关键词
铁锰矿床
地质特征
成矿机制
粤西
iron-manganese deposit
geological features
minerogenic mechanism
the west of Guangdong Province