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The primary geochemical characteristics of the Lanjia gold deposit in Jilin province

Han Yong-ji

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Abstract

The Lanjia gold deposit is located in the Daheishan banded horst of the Au-Ag polymetal ore-forming belt,in which has three types,i e skarn type,altered rock type in fracture zone and veinlet-disseminated type The formation of the ore deposit is closely related with the multiple actions of quartz diorite of the late Triassic Quanyangou succession(the south Quanyan unit) Au,Ag and Bi show the characteristics of metallogenic elements,and the primary geochemical characteristics can be an indicator for the evaluation of deposit and prospecting of ore deposits

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What this paper is about

The Lanjia gold deposit is located in the Daheishan banded horst of the Au-Ag polymetal ore-forming belt,in which has three types,i e skarn type,altered rock type in fracture zone and veinlet-disseminated type The formation of the ore deposit is closely related with the multiple actions of quartz diorite of the late Triassic Quanyangou succession(the south Quanyan unit) Au,Ag and Bi show the characteristics of metallogenic elements,and the primary geochemical characteristics can be an indicator for the evaluation of deposit and prospecting of ore deposits

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Available abstract

The Lanjia gold deposit is located in the Daheishan banded horst of the Au-Ag polymetal ore-forming belt,in which has three types,i e skarn type,altered rock type in fracture zone and veinlet-disseminated type The formation of the ore deposit is closely related with the multiple actions of quartz diorite of the late Triassic Quanyangou succession(the south Quanyan unit) Au,Ag and Bi show the characteristics of metallogenic elements,and the primary geochemical characteristics can be an indicator for the evaluation of deposit and prospecting of ore deposits

Key concepts: Geology, Skarn, Prospecting, Diorite, Geochemistry, Horst, Quartz, Polymetallic replacement deposit

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