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云南东川田坝矿区铅锌矿地质特征及找矿标志

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通过对田坝矿区铅锌矿床开展地质调查及研究,发现区内铅锌矿体产于中元古界昆阳群大营盘组第三段(Pt2d3)浅变质灰黑色绢云板岩中;区内Ⅰ、Ⅱ、Ⅲ、Ⅳ、Ⅴ号主矿体,属于铅锌矿第Ⅱ类勘查类型;矿体并明显受北北东向张扭性断裂及北西向压扭性断裂控制;矿石自然类型为原生硫化矿石;工业类型为铅锌易选矿石;矿床成因类型为断裂构造控制的中低温热液充填型铅锌矿床.
Geological characteristics and prospecting criteria of lead-zinc deposit in Tianba mining area,Dongchuan,Yunnan Province
Through geological investigation and research on the pb-Zn deposit in Tianba mining area,it is found that the PB-Zn deposit is located in the shallow metamorphic grayish-black sericornite SLATE of the third member of Daying Pan Formation(Pt2d3)in the Middle Proterozoic Kunyang Group.The main orebodies No.Ⅰ,Ⅱ,Ⅲ,Ⅳ and Ⅴ in the area belong to the Ⅱ exploration type of lead-zinc mine.The ore body is obviously controlled by the NE-trending tension-torsion fault and the NW-trending compression-torsion fault.The natural type of ore is primary sulfide ore.The industrial type is lead-zinc easy ore;The genetic type of the deposit is the middle-low temperature hydrothermal filling lead-zinc deposit controlled by fault structure.

lead-zinc orebrittle ductile structuresilicificationhydrothermal alteration

魏迎雨、樊培贺

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山东省地质矿产勘查开发局第六地质大队,山东 威海 264200

铅锌矿 脆韧性构造 硅化 热液蚀变

2024

世界有色金属
有色金属技术经济研究院

世界有色金属

影响因子:0.138
ISSN:1002-5065
年,卷(期):2024.(6)
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