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Fluid mixing as the mechanism of formation of the Dajing Cu-Sn-Ag-Pb-Zn ore deposit, Inner Mongolia : Fluid inclusion and stable isotope evidence

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Fluid mixing as the mechanism of formation of the Dajing Cu-Sn-Ag-Pb-Zn ore deposit, Inner Mongolia : Fluid inclusion and stable isotope evidence

Content Provider	Springer Nature Link
Author	Liu, Wei Li, Xinjun Tan, Jun
Copyright Year	2003
Abstract	Dajing Cu-Sn-Ag-Pb-Zn ore deposit, in the Inner Mongolia Autonomous Region of China, is a fissure-filling hydrothermal ore deposit. The δD values of quartz-hosted inclusion water are centered at −100%.– −130%.. The δ$^{34}$S values of sulfide ore minerals and δ$^{13}$ C values of carbonate gangue minerals vary from −0.3%. to 2.6%. and from −2.9%. to −7.0%., respectively. Integrated isotopic data point to two major contributions to the mineralizing fluid that include a dominant meteoric-derived groundwater, and sulfur and carbon species from hypogene magma. Linear trends are exhibited on the gaseous H$_{2}$O versus CO$_{2}$ plot, and plots of CO, N$_{2}$, CH$_{4}$, and C$_{2}$H$_{6}$. It is shown by quantitative simulation that magma degassing cannot explain the linear trends. Hence, these linear trends are interpreted in terms of mixing of CO$_{2}$-rich magmatic fluid with meteoric-derived groundwater. The groundwater circulated in Paleozoic sedimentary rocks and absorbed CO, N$_{2}$, CH$_{4}$, C$_{2}$H$_{6}$ and radiogenic Ar from organic matter. Cooling effects resulting from mixing have caused the precipitation of ore minerals.
Starting Page	652
Ending Page	663
Page Count	12
File Format	PDF
ISSN	10069313
Journal	Science in China Series D: Earth Sciences
Volume Number	46
Issue Number	7
e-ISSN	18622801
Language	English
Publisher	Science in China Press
Publisher Date	2003-01-01
Publisher Place	Beijing
Access Restriction	Subscribed
Subject Keyword	fluid mixing fluid inclusion quadrupole mass spectrometer stable isotope Dajing ore deposit Geosciences
Content Type	Text
Resource Type	Article
Subject	Earth and Planetary Sciences

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