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首页> 外文期刊>Chinese science bulletin >Age dating of lacustrine sedi - ments in Lake Tianshuihai of the Tibetan Plateau by using U-series isochron method and Its significance
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Age dating of lacustrine sedi - ments in Lake Tianshuihai of the Tibetan Plateau by using U-series isochron method and Its significance

机译:U序列等时法对青藏高原天水海湖相沉积物的年龄测年及其意义。

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摘要

The age of the clastic - clay sediments with var - ied content of carbonate in core TS95 taken from the Lake Tianshuihai in the northwest of the Tibetan Plateau was de - Termined successfully by using the total sample dissolution U-series isochron method for the first time. With this method, The serial absolute timescale (isotope time scale) covered the Last 240 ka in the main body of the Tibetan Plateau with a Sea level up to 4000 m is also established for the first time, Thereby laying the foundation for the research on the paleo - Climate and palaeoenvironment in the Lake Tianshuihai re - Gion as well as the relationship between evolution ofo the Ti - Betan Plateau and global changes.
机译:首次利用全样品溶解U系列等时线法成功地测定了来自青藏高原西北天水海的TS95岩心中碳酸盐含量变化的碎屑粘土沉积物的年龄。 。通过这种方法,还首次建立了青藏高原主体海域最后一个240 ka的序列绝对时标(同位素时标),海平面达4000 m,从而为进一步研究奠定了基础。天水海再入G园的古气候和古环境,以及贝塔高原的演变与全球变化之间的关系。

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