The development of fluvial systems on the southeastern margin of the Tibetan Plateau is
linked to significant and rapid late Cenozoic uplift. The relatively complete fluvial terrace …

Abstract The Yulin River in the northern Tibetan Plateau, consists of multiple
geomorphological features, including alluvial fans, fluvial terraces, and river profile …

Abstract The Yalong River is an important river that runs across the abruptly changing terrain
of the SE Tibetan Plateau. The terraces and Quaternary sediments in its valleys preserve the …

Abstract The substantial tectonic uplift (1000–2500 m in a few million years) of the
Northeastern Tibetan Plateau (NETP), together with the major climatic changes during the …

Understanding the processes of fluvial geomorphic evolution is based on thorough
evaluation of how rivers respond to tectonic activity and climatic change, with river terraces …

River terraces are significant geomorphic markers of climate and tectonics. However, the
competing roles of bedrock uplift and climatic change in the formation of fluvial terraces …

The uplift of the Tibetan Plateau was a significant event in terms of global landforms and
climate, but the exact nature of the uplift process remains contested among geologists. In the …

The Kunlun Range, a reactivated orogenic belt, constitutes the northern margin of the
Tibetan Plateau. The extreme relief and major landforms of the Kunlun Range are a product …

Spatiotemporal patterns of Cenozoic deformation along the margins of the Tibetan Plateau
can provide key evidence with which to investigate the mechanisms of continental …

Fluvial terraces are important archives for inferring changes in river dynamics. In the NE
Tibetan Plateau, the Huangshui River flows through broad depressions and narrow gorges …