Pliocene–Quaternary wind erosion profoundly modified the physiography of northern China
at a large range of spatial (10 m to> 100 km) and temporal (10 ka to Myr) scales. In the …

The age of the formation of the upper reaches of the Yellow River is controversial, ranging
from the Pliocene to the Middle Pleistocene. However, determining the source of the detrital …

Eolian sediments are extensively distributed across the Earth's surface, and their formation
is intricately linked to climate change, tectonic activity, and topographic features …

Continental-scale drainage reorganization is generally understood to result from landform
evolution forced by the coupling between tectonic activity and climate change, attracting …

Atmospheric mineral dust is a poorly constrained yet extremely important component of the
climate system. Provenance studies from geologic dust archives are crucial to understand …

Drainage divide migration, influenced by tectonic processes and climate change,
significantly shapes geomorphological dynamics and sediment dispersal patterns. However …

Abstract The Chinese Loess Plateau (CLP) in northern China is home to one of the most
prominent loess records in the world, reflecting past eolian dust activity in East Asia …

Atmospheric mineral dust is a fundamental component of the Earth's climate system, with
dust both responding to and driving climate change. This close link between dust and …