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- W2366154577 abstract "Under the pressure background for iron resource in our country, this paper detailedly study the Serblak iron deposit, following the wide exploration and study for iron deposits in Altay in Xinjiang.This iron deposit is situated in the contact zone between granite and embracing rock or xenoliths of stratoid in the southern margin in Altay.The geological characteristic indicates its typical skarn-type deposit.The study on fluid inclusion and stable isotope shows the middle-low temperature , low salinity and middle-low density fluid during mineralization, belonging to H2O-NaCl fluid.The deposit resulted from the metasomatism between Granitic magma and carbonate rock.Granitic magma derived from the deep melting of the mafic rock in oceanic crust during subduction in late Silurian -early Devonian when magmatic activity shows a peak in the southern margin in Altay, mixing with atmospheric water cycling in deep crust in the period of granitic magma ascending," @default.
- W2366154577 created "2016-06-24" @default.
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- W2366154577 date "2010-01-01" @default.
- W2366154577 modified "2023-09-25" @default.
- W2366154577 title "STUDY ON THE FLUID INCLUSION AND STABLE ISOTOPES FOR THE SAERBLAK IRON DEPOSIT IN ALTAY IN XINJIANG" @default.
- W2366154577 hasPublicationYear "2010" @default.
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