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- W2371297037 abstract "Hongdun and Tiemuerte lead-zinc deposits are all located in the Kelan rift basin of the middle part of the southern edge of Altai mountain,Xinjiang.Ore occurrences of two deposits are the same as the strata with obvious laminated bedding structure.There also exist some apparent differences between two deposits in geologic characteristics.For example,host rocks of Hongdun deposit is sedimentary clastic rock of Middle Devonian Aletaizheng Formation.Mineralization was related with marine basic volcanic rocks.There are more zinc-bearing minerals than lead-bearing minerals,and no copper-bearing mineral in the ores.Sphalerite is a low temperature one with lower iron.Host rock of Tiemuerte deposit is volcano clastic-carbonate rock of Lower Devonian Kangbutiebao Formation.Mineralization was related with marine acidic volcanic rocks.There are more lead-bearing minerals than zinc-bearing minerals,and more copper-bearing minerals ores.Sphalerite is high temperature ones with higher iron.Through the contrast study,it is thought that the Hongdun lead-zinc deposit belongs to SEDEX type,and the Tiemuerte lead-zinc deposit belongs to VHMS type." @default.
- W2371297037 created "2016-06-24" @default.
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- W2371297037 date "2006-01-01" @default.
- W2371297037 modified "2023-09-25" @default.
- W2371297037 title "CONTRAST BETWEEN HONGDUN AND TIEMUERTE LEAD-ZINC DEPOSITS IN THE KELAN BASIN,XINJIANG" @default.
- W2371297037 hasPublicationYear "2006" @default.
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