河南省卢氏县张家山铁矿地质特征及成因浅析  

Geological Characteristics and Genesis of Zhangjiashan Iron Deposit in Lushi County,Henan Province

作　　者：周红春[1] 刘传权[1] 郭克剑 彭松民[1] 张毅星[1] 王凌云[1] 

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

出　　处：《华南地质与矿产》2008年第2期43-48,共6页Geology and Mineral Resources of South China

摘　　要：通过对张家山铁矿床矿体与围岩的接触关系、蚀变特征、矿石的矿物组合、化学组分等地质特征及成因的分析研究,认为张家山铁矿床应属风化淋滤型铁矿床,其原生矿床为铁多金属硫化物矿床,并厘定了该地区铁矿的找矿标志。Through the study of the relationship between the ore bodies and the country rocks, alteration, mineral association and chemical constituents in Zhangjiashan Iron Deposit, we think that Zhangjiashan Iron Deposit should be classified as weathering leaching type iron deposit, and the primary deposit should be a Fe polymetallic deposit. We have still collated and stipulated the indicators of iron deposit in this area.

关 键 词：地质特征 矿床成因 找矿标志 张家山铁矿 

分 类 号：P618.31[天文地球—矿床学]