中国黄土高原的黄土，作为全球变化研究的信息载体，是连续性最好、蕴藏信息最丰富的第四纪陆相沉积物。
As a information carriers of the research of global change, the loess in Chinese loess Plateau is the most consecutive sediment and has the most abundance information since Quaternary.
唐古拉山地区广泛出露早新生代陆相地层，较好地记录了青藏高原北部新生代地质构造演化与古环境变迁的过程。
The Cenozoic fluvial strata, exposed widely in the Tanggula Mountains, detaily recorded the information of the uplift of the northern Tibet Plateau and the paleoenvironmental evolution.
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