河南省嵩县小公峪矿区构造破碎带型金矿体特征及成因分析  

Analysis of the Characteristics and Genesis of Tectonoclastic Zone-type of Gold ore body of Xiaogongyu Mining Area in Song County,Henan Province

作　　者：郭克剑 刘传权[2] 周红春[2] 

机构地区：[1]河南地矿建设工程集团公司,郑州450000 [2]河南省地质调查院,郑州450051

出　　处：《华南地质与矿产》2008年第2期9-14,共6页Geology and Mineral Resources of South China

基　　金：国土资源部地质大调查项目(200213000035)资助

摘　　要：通过对金矿特征分析,认为小公峪矿区金矿主要受构造破碎带控制。根据硫、铅同位素及稀土元素分析结果,该金矿成矿物质主要来源于燕山期花岗岩浆,成因为燕山晚期岩浆热液型中低温矿床。Through the analysis of the characteristics of Xiaogongyu gold mine, we think it is mainly controlled by the tectonic zone. According to the analytic results of the Sulfur isotopes, Lead isotopes and REE, we think that the gold mine minerals mainly came from the granitic magma during the stage of Yanshanian. The genesis of this gold mine is magmatic hydrothermal deposits in the middle - low temperature of the late stage of Yanshanian.

关 键 词：金矿特征 构造破碎带 成因分析 燕山期花岗岩浆 

分 类 号：P618.51[天文地球—矿床学]