The occurrence of endorheic basins on the Tibetan Plateau, both in its Pleistocene history
and (fewer in number) at the present day, has been attributed to the 'basin-and …

Increased exposure to arsenic (As) has been reported in many arid and semi-arid areas,
where drinking water and agricultural irrigation strongly rely on groundwater. High-As …

Based on the case studies and new progresses of river evolution in recent years around the
world, this paper introduces the main research carriers and ideas applied to the study of …

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 …

Upstream knickpoint propagation is an essential mechanism for channel erosion, carrying
changes in base level, tectonics and climate across the landscape. Generally, the terraces …

Understanding the formation of the Qilian Shan in the NE Tibetan Plateau provides insights
into the growth mechanisms of the northern portion of the plateau through time. The onset …

The geomorphic evolution of the Yellow River, especially its upper reach, contains critical
information on the tectonic activity and climatic change within and around the northeastern …

Reconstructing and interpreting past hydrological system changes from the Quaternary
sediment-landform record presents many challenges especially when trying to establish …

本文基于近年来全球河流地貌演化的研究实例及新进展, 介绍了主要的研究载体与思路,
讨论了河流地貌演化事件背后的地质, 环境意义. 沉积学, 地貌学, 物源分析 …

Abstract The Yellow River (YR) flows from Northwest China to North China, crossing three
topographic steps: the Tibetan Plateau, the Chinese Loess Plateau (CLP), and the North …