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THE METALLOGENETIC CHARACTERISTICS AND ORE PROSPECTING MARKS OF LUJIACUN AG-AU MULTIMETALLIC DEPOSIT,XIANGGELILA

Huiqin Huang

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Abstract

In the shallow part of study area,the ore deposit is mainly the hydrothermal Cu,Au,Pb,Ag veined deposit controlled by fault zone,whereas the porphyry Cu,Mo deposit in the deep part.The ore bodies are controlled dually by strata and fault structure.The silisification,pyritization(limonitization)are in close relation with the metallogenesis,which are the main alteration of wall rock and the main marks in ore prospecting.

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What this paper is about

In the shallow part of study area,the ore deposit is mainly the hydrothermal Cu,Au,Pb,Ag veined deposit controlled by fault zone,whereas the porphyry Cu,Mo deposit in the deep part.The ore bodies are controlled dually by strata and fault structure.The silisification,pyritization(limonitization)are in close relation with the metallogenesis,which are the main alteration of wall rock and the main marks in ore prospecting.

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Available abstract

In the shallow part of study area,the ore deposit is mainly the hydrothermal Cu,Au,Pb,Ag veined deposit controlled by fault zone,whereas the porphyry Cu,Mo deposit in the deep part.The ore bodies are controlled dually by strata and fault structure.The silisification,pyritization(limonitization)are in close relation with the metallogenesis,which are the main alteration of wall rock and the main marks in ore prospecting.

Key concepts: Prospecting, Geology, Hydrothermal circulation, Geochemistry, Fault (geology), Contact zone, Mining engineering, Paleontology

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THE METALLOGENETIC CHARACTERISTICS AND ORE PROSPECTING MARKS OF LUJIACUN AG-AU MULTIMETALLIC DEPOSIT,XIANGGELILA — Research Paper | ScholarLens