CAJ | 학술논문

秦家庄钛铁矿床赋存于古元古代红门超单元三官寨单元中粗粒角闪辉长岩中，并严格控制了矿体的展布状态。矿体形态简单，规模大，为岩浆分异-变质改造型矿床。本文通过地质背景、地球物理特征、矿床地质特征、矿石类型等分析了矿床成因，建立了找矿标志。为同类矿床的勘查及促进资源的综合利用具有一定的指导意义。
진가장태철광상부존우고원고대홍문초단원삼관채단원중조립각섬휘장암중，병엄격공제료광체적전포상태。광체형태간단，규모대，위암장분이-변질개조형광상。본문통과지질배경、지구물리특정、광상지질특정、광석류형등분석료광상성인，건립료조광표지。위동류광상적감사급촉진자원적종합이용구유일정적지도의의。
Qin Jia Zhuang ilmenite occurrence of the paleopro-terozoic Red Gate's extra bed unit Chai unit of three coarse angle Flash gabbroic, and strictly control the distribution of orebodies. Sim-ple habit, large scale, for magma differentiation-metamorphic transfor-mation-type deposits. Through geological setting, geophysical charac-teristics and geological characteristics, ore types, such as analysis of Genesis, the establishment of a prospecting. Similar deposit prospect-ing for and promoting the comprehensive utilization of resources has some significance.