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- W2362898501 abstract "Quantitative inversion of palaeo-temperatures of lake water and atmosphere can promote the past global change research from qualitative to quantitative.Three main methods with lacustrine carbonates have been used to reconstruct the lake water palaeo-temperature at present.First,the technique of isotopic geological thermometer,since being put forward to reconstruct sea-water paleo-temperature,was subsequently introduced into lacustrine carbonate sediments for constructing lake-water based upon the function relationship between lake-water temperature and the oxygen isotopic compositions of lacustrine carbonate and lake-water.Second,paleo-temperature of the lake-water can be reconstructed by determining Mg/Ca values of the lacustrine ostracode shells.And third,paleotemperature of the lake-water can be reconstructed based upon the statistic model between the oxygen isotopic composition of lacustrine carbonate and the lakewater temperature by testing the modem hydrogeological parameters and some relevant isotopic data of the lake basin.Each method has its own applicable condition,scope and limitation,and all of these points are reviewed and discussed in this paper." @default.
- W2362898501 created "2016-06-24" @default.
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- W2362898501 date "2008-01-01" @default.
- W2362898501 modified "2023-09-26" @default.
- W2362898501 title "Quantitative Research Progress on Palaeo-temperatuer Inferred from Lacustrine Carbonates" @default.
- W2362898501 hasPublicationYear "2008" @default.
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