Age dating of lacustrine sediments in Lake Tianshuihai of the Tibetan Plateau by using U-series isochron method and its significance

The age of the clastic clay sediments with varied content of carbonate in c ore TS95 taken from the Lake Tianshuihai in the northwest of the Tibetan Pl ateau was determined successfully by using the total sample dissolution U-s eries isochron method for the first time. With this method, the serial abso lute timescale (isotope time scale) covered the last 240 ka in the main bod y 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 p aleoclimate and palaeoenvironment in the Lake Tianshuihai region as well as the relationship between evolution of the Tibetan Plateau and global chang es, In addition to a brief introduction of the basic principles, the proced ures of experiments, and the results, this note also presents the adaptabil ity and superiority of this method as well as its possible problems.