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- W2385560545 abstract "The Huize superlarge Pb-Zn ore deposit is characterized by its bi g scale, high contents of Pb+Zn and multiple concomitant elements, which shows th at its ore-forming condition is relatively special. This paper analyzes the car bon and oxygen isotopic compositions of calcites occurring as gangue mineral in ores and in carbonate strata that host the ores. The results show that the carbo n and oxygen isotopic compositions of the calcites are relatively homogeneous, a nd the carbon and oxygen isotopic compositions of the calcites that appear in di fferent ore bodies, have different occurrences and the same ore body with varied occurrences are not obviously different from one another. The values of ?13CPD B and ?18OSMOW of calcite range respectively from-2.1‰～-3.5‰(the average value is-2.8‰) and 16.7‰～18.6‰(the average value is 17.7‰). In the ?13CP DB vs ?18OSMOW diagram, the samples are plotted in a small field between carbon atite and marine carbonate. A variety of evidences demonstrate that the ore-for ming fluids are of the crustal-mantle mixing type, with the crustal composition s being mainly originated from the carbonate strata in the orefield, and the man tle compositions being related to the degassing process of the Emeishan basalt m agmatism." @default.
- W2385560545 created "2016-06-24" @default.
- W2385560545 creator A5005228989 @default.
- W2385560545 date "2004-01-01" @default.
- W2385560545 modified "2023-09-25" @default.
- W2385560545 title "CARBON AND OXYGEN ISOTOPE GEOCHEMISTRY OF THE HUIZE SUPERLARGE Pb-Zn ORE DEPOSITS IN YUNNAN PROVINCE" @default.
- W2385560545 hasPublicationYear "2004" @default.
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