▪ Abstract Accumulation rates of terrestrial sediment have increased in the past few million
years both on and adjacent to continents, although not everywhere. Apparently, erosion has …

Compressional intracontinental orogens are major zones of crustal thickening produced at
large distances from active plate boundaries. Consequently, any account of their initiation …

We address the problem of late Cenozoic uplift, erosion, and growth of northeastern Tibet by
reconstructing, from isopach maps and drill holes, the volumes and masses of sediments …

The timing of uplift of the Tibet Plateau has a central role in the development of tectonic
models for the Tibet Plateau and Cenozoic global climate change. A detailed …

During the Mesozoic, the active southern margin of Eurasia was the site of several accretion
and collision events that fit into a framework of convergence between Eurasia and …

This work establishes estimates of mass accumulation rates in 18 mostly offshore
sedimentary basins in Asia since the beginning of the Cenozoic,≈ 66 Ma. The estimates …

We present the results of mapping selected cross-sections across the margins of the
Chinese Tien Shan, an intracontinental mountain belt that formed in response to the India …

The Cenozoic Tian Shan is one of the preeminent examples of an intracontinental orogen.
However, there remains a significant controversy over when deformation related to the India …

Abstract The Tien Shan are the quintessential intracontinental range, situated more than
1000 km north of the suture between India and Asia. Their initiation and growth in the …

Low internal relief, aridity, and internal drainage characterize the Puna‐Altiplano Plateau
and the Tibetan Plateau and the Tarim basin. Structurally, these areas are reverse fault …