Geological Characteristics and Genesis of Huangpuling Gold Deposit in Shandong Provice
Zhang Yuan
Abstract
Zhang Yuan
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.
A significance statement is not available in the OpenAlex record.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
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