河北承德张营子钒钛磁铁矿床地质特征与成因浅析  

Analysis of Geological Features and the Genesis of Vanadium Titanium Magnetite Deposit in Zhangyingzi,Chengde City,Hebei Province

作　　者：赵向奎 王瑞权[1] 张立剑[1] 王晓东 ZHAO Xiang-kui;WANG Rui-quan;ZHANG Li-jian;WANG Xiao-dong(The Fourth Geological Division,Hebei Bureau of Geology and Mineral Resources Exploration,Chengde,Hebei 067000,China)

机构地区：[1]河北省地质矿产勘查开发局第四地质大队,河北承德067000

出　　处：《企业技术开发》2018年第10期78-81,共4页Technological Development of Enterprise

摘　　要：张营子钒钛磁铁矿床位于红石砬—大庙—娘娘庙深断裂南侧,产于超基性岩体内,受区域次级构造控制,侵入于晚太古代变质岩中,矿床成因为岩浆晚期分异式铁矿。Zhangyingzi Vanadium-titanium magnetite deposit is located on the south side of the deep fracture of the Hongshila-- Damiao-Niang Niang Temple,which originated in the ultrabasicrock body and is controlled by the regional secondary structure. It invades into the late Archeozoic metamorphic rock.The genesis of deposit is due to the differentiation of iron ore deposit in the late phase of magmatic.

关 键 词：超基性岩 钒钛磁铁矿 地质特征 矿床成因 

分 类 号：P618[天文地球—矿床学]