A Tentative Discussion on Ore-Forming Material Sources and Mineralization of Shanggong Gold Deposit in Western Henan Province
Through lots of field geological investigation and interior comprehensive analysis, discussion on ore-forming material sources and mineralization of the ShangGong gold deposit in western Henan Province, preliminary considered that ShangGong area is a typical mantle branch structure, which is the main mineralization and ore-controlling structure.The deep origin ore-forming fluid along XiongEr Mountain mantle branch structure shaft fracture upwelling moved to the mantle branch structure detachment zone of JinDongGou fracture, redox environment prompted the ore-forming elements precipitated in structural extension zone, concentration in ore-forming.The article taking the mantle branch structure theory as guidance, through the analysis of spatial distribution regularity of orebody, metallogenic geological characteristics, structural ore controlling regularity, established metallogenic evolution model, provided evidence for the deep and periphery prospecting.
Mantle branch structure Mineralization Material source Gold deposit Western Henan area
SONG Kai WANG Jianghe HAO Xiaoyuan
Shijiazhuang University of Economics,Hebei,China The 1st Geological Team of Henan Geological Exploration and Exploitation Buren,Luoyang,Henan,China
国际会议
第十八届凯洛林国际地质学术研讨会(The 18th Kerulien International Conference on Geological)
石家庄
英文
202-206
2013-09-20（万方平台首次上网日期，不代表论文的发表时间）