Abstract The Youjiang Basin in the western part of the South China Block (SCB), preserves
the records of the tectonic history from Tethyan, through Paleo-Pacific to Tibetan domains …

Existing end-member models sparked debates concerning plateau formation in the
southeast Tibetan Plateau through early-middle Cenozoic transpressional and shortening …

The southeast margin of the Tibetan plateau is characterized by deeply incised river valleys
separated by a perched low relief landscape that gently descends from the high Tibetan …

Combining 121 new fission track and (U‐Th)/He ages with published thermochronologic
data, we investigate the Late Cretaceous‐Cenozoic exhumation/cooling history of the …

Abstract The Longmenshan Tectonic Complex (LSTC), along the eastern margin of the
Tibetan Plateau, the site of devastating earthquakes such as the magnitude 8.0 (Wenchuan) …

The geometry and evolution of fluvial systems are thought to be related to surface uplift. In
eastern Tibet, rivers exhibit peculiar drainage patterns but how these patterns were …

Abstract The Tibetan Plateau is characterized by high elevation and complex fault systems.
High‐precision vertical movement data can provide important constraints for understanding …

Synchronous response of river erosion to surface uplift is often assumed by studies using
thermochronometer‐constrained erosion histories to estimate changes in landscape and …

A large part of the southeastern Tibetan Plateau (TP) is characterized by low‐relief surfaces
at high elevations (> 3.5 km). The origin of these landscapes and their geodynamic …

Abstract Epizonal orogenic Au‐Sb deposits are generally Phanerozoic in age, possibly as a
consequence of erosion that can entirely remove older mineral deposits in rapidly uplifting …