甘肃夏河三索玛金矿地质特征及成因探讨  

Gansu Xiahe Gold Mine Geological Characteristics and Genetic Discussion of Sansuoma

作　　者：邵小鹏[1] SHAO Xiao-peng(The Third Institute of Geology and Minerals Exploration, Gansu Provincial Bureau of Geolgy and Minerals Exploration and Development, Lanzhou 730050, Chin)

机构地区：[1]甘肃省地矿局第三地质矿产勘查院,甘肃兰州730000

出　　处：《甘肃冶金》2018年第3期36-41,共6页Gansu Metallurgy

摘　　要：以三索玛金矿床为研究对象,在充分野外地质调查和前人工作的基础上,通过对历年来三索玛一带勘查成果总结分析,认为三索玛金矿矿床产出于洒索玛岩体的外接触带上,矿体严格受北东向和南北向断裂破碎带及其次级裂隙的控制,为一典型构造破碎蚀变岩型金矿床,具较好找矿潜力。This paper gold deposits of Sansuoma as the research object,in full field geological survey and the basis of previous work,through over the area of exploration results analysis,think gold ore deposits of Sansuoma in the rock mass with output POTS clatters loudly the contact of take,ore body strictly by north east to and north and south to fractured zone and its control of the subprime fractures,and is a typical broken tectonic altered rock type gold deposits,with good prospecting potential.

关 键 词：金矿床 矿床特征 矿床成因 三索玛 

分 类 号：P618.51[天文地球—矿床学]