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- W2365202232 abstract "Based on the experimental analysis of strontium isotope composition on marine carbonate of Leikoupo formation in Pingluo No.4 well core samples,the matter source supply of halogen-bearing carbonate strata and the sedimentary environment were studied in this paper,and the impact of later deep hydrothermal activity on brine forming was discussed.The results show that: The change of marine carbonate w(87Sr)/w(86Sr) is mainly affected by the the eruption of the emei mountain basaltic magma occurred in the later permian and tectonic uplifting in indosinian which changed sichuan from the ocean basin to single basin;substances derived from the deep risen along the fault zone at late stage,changed the relative proportions of the Sr source in the initial carbonates and made w(87Sr)/w(86Sr) lower in part layers;the energy brought by hydrothermal activities heated some strata and the brines and conduced to the decomposition of polyhalite beds and other potassium-bearing minerals,which gave rise to more enrichment of potassium ions in brines." @default.
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- W2365202232 date "2011-01-01" @default.
- W2365202232 modified "2023-09-27" @default.
- W2365202232 title "Strontium Isotope Geochemical Characteristics of Marine Carbonate on Leikoupo Formation in Pingluo,West Sichuan" @default.
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