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Study on metallogenic conditions and occurrence regularityof Luziyuan Pb-Zn deposit,Zhengkang Town,Yunnan Province

LV Changlian

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Abstract

Luziyuan Pb-Zn deposit in,Zhenkang Town,Yunnan Province is asuper-large polymetallic deposit discovered in recent years.The ore body mainly occurs in Upper Cambrian Shahechang formation and is controlled by NE faults and the associated sub-structures.Spatially,the ore bodies are plunged and distributed in equal distance.Wall-rock alterations are developed.Mineralization is dived into meso-epithermal stage and mesothermal-high temperature stage.Where marblization,skarnization,pyritization, silicification are developed and overprinted mineralization is strong.Ore materials are mainly derived from the ore-bearing strata and the deeply seated intrusive body.Based on study on lithologies of ore-bearing strata,the ore-control fracture,wall rock alteration and the ore fabric,the deposit is related to multistaged tectonic movement and magmatic hydrothermal fluid and is a hydrothermal-skarn type Pb-Zn-Fe polymetallic deposit.

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What this paper is about

Luziyuan Pb-Zn deposit in,Zhenkang Town,Yunnan Province is asuper-large polymetallic deposit discovered in recent years.The ore body mainly occurs in Upper Cambrian Shahechang formation and is controlled by NE faults and the associated sub-structures.Spatially,the ore bodies are plunged and distributed in equal distance.Wall-rock alterations are developed.Mineralization is dived into meso-epithermal stage and mesothermal-high temperature stage.Where marblization,skarnization,pyritization, silicification are developed and overprinted mineralization is strong.Ore materials are mainly derived from the ore-bearing strata and the deeply seated intrusive body.Based on study on lithologies of ore-bearing strata,the ore-control fracture,wall rock alteration and the ore fabric,the deposit is related to multistaged tectonic movement and magmatic hydrothermal fluid and is a hydrothermal-skarn type Pb-Zn-Fe polymetallic deposit.

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Available abstract

Luziyuan Pb-Zn deposit in,Zhenkang Town,Yunnan Province is asuper-large polymetallic deposit discovered in recent years.The ore body mainly occurs in Upper Cambrian Shahechang formation and is controlled by NE faults and the associated sub-structures.Spatially,the ore bodies are plunged and distributed in equal distance.Wall-rock alterations are developed.Mineralization is dived into meso-epithermal stage and mesothermal-high temperature stage.Where marblization,skarnization,pyritization, silicification are developed and overprinted mineralization is strong.Ore materials are mainly derived from the ore-bearing strata and the deeply seated intrusive body.Based on study on lithologies of ore-bearing strata,the ore-control fracture,wall rock alteration and the ore fabric,the deposit is related to multistaged tectonic movement and magmatic hydrothermal fluid and is a hydrothermal-skarn type Pb-Zn-Fe polymetallic deposit.

Key concepts: Geology, Mineralization (soil science), Geochemistry, Skarn, Mesothermal, Hydrothermal circulation, Polymetallic replacement deposit, Lithology

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Study on metallogenic conditions and occurrence regularityof Luziyuan Pb-Zn deposit,Zhengkang Town,Yunnan Province — Research Paper | ScholarLens