Abstract As the largest Mesozoic-Cenozoic terrestrial intermountain basin in the northern
Tibetan Plateau, the Qaidam Basin is an ideal basin to examine the influences of regional …

Global cooling and the uplift of the Tibetan Plateau have long been considered the crucial
controls of the climate change in inland Asia since the Cenozoic. However, which of these …

Abstract The Qaidam Basin, located on the northeastern Tibetan Plateau and containing
Cenozoic sediments with a maximum thickness of~ 12,000 m, is an ideal place to study the …

Obtaining a continuous sedimentary record of Cenozoic East Asian paleoclimate change is
key to understand the origin, evolution and driving mechanism of the East Asian monsoon …

The initial aridification of mid-latitude Asia is thought to be one of the most prominent
Cenozoic environmental changes in Asia. However, precisely dated, fine-grained sediments …

古气候是陆相湖盆层序地层形成的主要沉积动力学因素之一. 古-新近纪柴北缘西段及周边地区
古气候演化过程复杂, 目前就古气候演化过程还存在争议, 利用地球化学方法对重点井的岩心和 …

A better understanding of the Cenozoic source to sink relationship between the Qaidam
Basin and the surrounding regions allows us to reveal the topographic evolution of the …

Clay mineralogy and elemental geochemistry of lacustrine sedimentary records have been
widely used in paleo-weathering and paleo-climate studies. However, different paleo …

Lithium isotopes have great potential to fractionate at subaerial environment, so they are
promising proxies for tracing chemical weathering history. However, it remains uncertain …

A thorough understanding of sub-decadal paleoclimate variability typically depends on ultra-
precise geochronological constraints that are rarely obtained. While the seasonally resolved …