鄂东矽卡岩型铁(铜)矿床模式及品位、吨位模型探讨  

Genetic pattern and ton-grade model of skarn Fe-Cu deposit in eastern Hubei Province

作　　者：孙立杨[1] 苏欣栋[1] 

机构地区：[1]中南冶金地质研究所,湖北宜昌443003

出　　处：《华南地质与矿产》2004年第2期27-31,共5页Geology and Mineral Resources of South China

摘　　要：通过对矽卡岩型铁(铜)矿床的研究对比,建立了鄂东独特的矽卡岩型铁(铜)矿床模式及品位、吨位模型。应用模型进行定量预测,反映该类矿床在鄂东有较大找矿前景。提出程潮矿床东南部的深部、灵乡岩体中部蜡烛山地段和金山店南陈家湾地段为预测区。In the light of contrastive study, genetic pattern and ton-grade models of skarn Fe-Cu deposits in eastern Hubei Province have be built. Quantitative prediction with these models show that deposits of this kind in the study area have large prospecting foreground,especially in the southeastern deep part of the Chengchao Fe-Cu deposit,Lazhu area in the central part of the Lingxiang granitic body and Chenjiawan area in southern part of Jinshandian.

关 键 词：矽卡岩型铁(铜)矿床 矿床模式 品位、吨位模型 鄂东 

分 类 号：P618.31[天文地球—矿床学] P618.41[天文地球—地质学]