地质与资源2018，Vol.27Issue(3)：251-256,6.
内蒙古扎赉特旗神山铁铜矿床地质特征及找矿标志
GEOLOGICAL CHARACTERISTICS AND PROSPECTING INDICATORS OF THE SHENSHAN IRON-COPPER DEPOSIT IN JALAID QI, INNER MONGOLIA
摘要
Abstract
The Shenshan Fe-Cu deposit in Inner Mongolia is of typical skarn type in the middle section of Daxinganling metallogenic belt. Two contact zones from north to south occur around Yilite intrusion and the residual Zhesi formation inside the intrusion, generally distributed in NE 45-50° with lengths about 1200 m and 3000 m, respectively, from east to west. The orebodies are hosted in the skarn dominated by epidote and garnet in the contact zone, while partially distributed in faults or interlayer detachment faults of exocontact zones. Altogether 22 orebodies including 7 main orebodies are delineated with single characterized by small-scaled, complex shape and high iron content.关键词
神山铁铜矿床/地质特征/夕卡岩型/大兴安岭中段/内蒙古Key words
Shenshan Fe-Cu deposit/geological characteristics/skarn type/middle section of Daxinganling Mountains/Inner Mongolia分类
天文与地球科学引用本文复制引用
吕骏超,刘桂香,张德宝,谭红艳,赵岩,毕中伟..内蒙古扎赉特旗神山铁铜矿床地质特征及找矿标志[J].地质与资源,2018,27(3):251-256,6.基金项目
中国地质调查局项目"内蒙古扎赉特旗新林-神山地区矿产地质调查"(编号12120113055600),"大兴安岭成矿带漠河-扎兰屯地区地质矿产调查"(编号DD20160047). （编号12120113055600）
