摘要
先锋硫铁矿位于宜宾市兴文县。先锋硫铁矿主要矿石矿物为黄铁矿、白铁矿、胶黄铁矿;脉石矿物:高岭石、珍珠陶土等。矿石结构:半自形-自形晶粒结构、它形粒状结构、碎裂结构、变胶状环带结构;矿石构造:浸染状、条带状、网脉状、根须状、树枝状、团块状、结核状等构造。分析将从古地形初始、硫铁矿表生富集和硫铁矿成岩富集三个阶段。
Xianfeng pyrite is located in Xingwen County, Yibin City. The main ore minerals of Xianfeng pyrite are pyrite, white iron ore, colloidal pyrite, gangue minerals: Kaolinite, pearl clay and so on. Ore structure: semi-self-shaped and self-shaped grain structure, its grain structure, fragmentation structure,variable colloidal ring structure, ore structure: disseminated, banded, reticulated vein, root whisker, dendritic, mass, tuberculosis and so on. The analysis will be carried out from three stages: the initial palaeotopography, the epigenetic enrichment of pyrite and the diagenetic enrichment of pyrite.
引文
[1]李昱臻,徐长昊,吴小艳.四川叙永两河口硫铁矿矿石特征及成矿作用分析[J].中国非金属矿工业导刊, 2015(1):46-49.
[2]陈荣骏.四川省兴文县先锋硫、煤矿区周家矿段详细勘探地质报告[R].四川省地矿局202地质队, 1985.
[3]李瑞玉.川南硫铁矿特征与富集规律[J].化工矿山技术,1983(S1):5-8.