摘要
半山磁铁矿位于会理-会东铜、铁、铅、锌、金成矿带内。矿体赋存于前震旦系会理群力马河组第三段绿泥阳起片岩、绢云母石英片岩中,呈似层状、透镜状产出,受层位、岩性及构造控制。矿石主要为低品位磁铁矿。矿床属于变质热液型。矿区磁铁矿石品位低,但规模大、低硫、低磷,易采、易选。该文通过对矿床区域地质背景、矿区地质、矿体特征、矿石质量的分析,对矿床控矿因素、成因、找矿标志进行了讨论,认为该矿区成矿地质条件好,找矿潜力大,并提出了下一步找矿方向。
The Banshan magnetite deposit is located in the Huili-Huidong Cu-Fe-Pb-Zn-Au metallogenic belt.The orebodies occur as stratoid and lenticular form in chlorite-actinolite schist and sericite-quartz schist in the Third Member of the Limahe Formation of the Huili Group of the Pre-Sinian System and are controlled by the horizon,lithology and structure.The deposit belongs to metamorphic hydrothermal type.The ore is mainly composed of magnetite and characterized by low grade,low S,low P and easy to be mined and selected.The ore control factors,genesis and ore criteria of the deposit are discussed on the basis of which its range of reconnaissance is put forward.
作者
李利
凌培平
LI Li;LING Pei-ping(The 281st Geological Party,Sichuan Bureau of Uranium Geology,Xichang,Sichuan 614500)
出处
《四川地质学报》
2022年第1期45-49,共5页
Acta Geologica Sichuan
关键词
磁铁矿
地质特征
找矿方向
半山
会理
magnetite
geological feature
range of reconnaissance
Banshan,Huili