The study of large-scale and long-term sedimentary hiatus and exhumation in vast intraplate
basins is of great significance for unravelling their tectonic development, morphodynamics …

The evolution of rivers is closely tied to basin tectonics and climate change. Consequently,
understanding the formation and evolution of large rivers (which can traverse diverse …

Abstract Across the Miocene–Pliocene boundary (MPB; 5.3 million years ago, Ma), late
Miocene cooling gave way to the early-to-middle Pliocene Warm Period. This transition …

Formation and evolution of the Asian landform was determined by growth of the Himalaya-
Tibetan Plateau and evolution of the Asian monsoon climate during the Cenozoic period. In …

The incision of the Sanmen Gorge marks the birth of the modern Yellow River, but its timing
varies from the late Miocene-early Pliocene to the late Pleistocene (∼ 0.15 Ma), and the …

The lateral movement of drainage divides is co-influenced by tectonics, lithology, and
climate and therefore archives a wealth of geologic and climatic information. It also has wide …

The formation of magma‐poor continental rifts is an enigmatic process, as the weakening
mechanism (s) for cratonic lithosphere remains uncertain in the absence of elevated …

Continental intraplate basalts usually exhibit diverse compositions varying from silica-
deficient alkaline basalts to silica-excess tholeiites. However, the mechanism of …

It is generally agreed that the channel‐head steady‐state elevations (zs) across a drainage
divide are different when the drainage divide is moving. However, whether it is the hillslope …

The stability of drainage divides is widely used for tectonic reconstruction. A drainage divide
migrating from the high-uplift side towards the geometric center is usually thought to indicate …