Holocene climate controls on water isotopic variations on the northeastern Tibetan Plateau
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摘要
<正>Although stable isotopes derived from lake sediments around the Tibetan Plateau have been widely used for reconstructions of past hydroclimate variations,the interpretation of the isotopic data is further complicated by multiple factors influencing isotopic fractionation,such as temperature effect and amount effect on precipitation isotopes,evaporation effect under dry climate(including evaporation on lake water,rain drops,
引文

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