Reorganization of the Asian climate from one dominated by global planetary wind systems
to a regional monsoon climate is closely related to the surface uplift of the Tibetan Plateau …

Silicate weathering is critical to global carbon cycle and climate change, and has attracted
considerable attention in Earth science studies. Chemical weathering intensity evaluation …

Accurately reconstructing the evolution of the Asian monsoon is predicated on
understanding the impact of temperature, precipitation, and tectonic paleogeography on …

The Cenozoic history of aridification in the Asian interior is thought to be intimately linked to
uplift of the Tibetan Plateau and long-term global cooling. How fluctuating climatic conditions …

Chemical weathering of continental silicates is a crucial geological process in regulating
Earth's long-term climate and participating in global carbon cycle. The increasing aridity and …

含铀岩系沉积时的古气候条件对铀成矿起着重要的控制作用, 但是长期以来未引起人们足够重视
. 以松辽盆地西南部HLJ 地区含矿目的层姚家组下段为研究对象, 通过对代表性钻孔岩心的泥岩 …

Sediment source-to-sink history is pivotal to investigating the evolution of ancient
sedimentary basin. Previous study focuses mostly on reconstruction of various components …

Cretaceous terrestrial sedimentary records are crucial for our understanding of geological
systems' responses to past climate change under greenhouse condition. Numerous …

The relationship between silicate weathering, Tibetan Plateau uplift, and global cooling
during the Cenozoic provides a valuable case study for understanding the interaction of …

The X-ray fluorescence (XRF) core-scanned Rb/Sr ratios of lake sediments have been
widely used as a proxy for chemical weathering intensity and past climate change. However …