2007•Geology and Mineral Resources of South ChinaRequires access

Geological Characteristics and Genesis of Huangpuling Gold Deposit in Shandong Provice

Zhang Yuan

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Abstract

On the basis of regional geology and ore deposit geology,by test studying sulfur isotope,hydrogen oxygen isotope and fluid inclusion.Tthe mineralization genesis of Hangpuling gold deposit is belong to hydrothermal ore band,controlled by structure,granite,dyke,altered rock etc.Mineralization temperature is medium temperature(160℃~350℃).Analysis of stable isotope,the sulfur is from deep stratum,and magma water and atmospheric water maxed during the ore formation.At last,the Huangpuling gold deposit belongs to medium temperature magma hydrothermal deposit.

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On the basis of regional geology and ore deposit geology,by test studying sulfur isotope,hydrogen oxygen isotope and fluid inclusion.Tthe mineralization genesis of Hangpuling gold deposit is belong to hydrothermal ore band,controlled by structure,granite,dyke,altered rock etc.Mineralization temperature is medium temperature(160℃~350℃).Analysis of stable isotope,the sulfur is from deep stratum,and magma water and atmospheric water maxed during the ore formation.At last,the Huangpuling gold deposit belongs to medium temperature magma hydrothermal deposit.

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Available abstract

On the basis of regional geology and ore deposit geology,by test studying sulfur isotope,hydrogen oxygen isotope and fluid inclusion.Tthe mineralization genesis of Hangpuling gold deposit is belong to hydrothermal ore band,controlled by structure,granite,dyke,altered rock etc.Mineralization temperature is medium temperature(160℃~350℃).Analysis of stable isotope,the sulfur is from deep stratum,and magma water and atmospheric water maxed during the ore formation.At last,the Huangpuling gold deposit belongs to medium temperature magma hydrothermal deposit.

Key concepts: Geology, Hydrothermal circulation, Geochemistry, Mineralization (soil science), Sulfur, Stratum, δ34S, Magmatic water

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