High-pressure low-temperature (HP–LT) metamorphic rocks provide invaluable constraints
on the evolution of convergent zones. Based on a worldwide compilation of key information …

With its central position between the Tibetan Plateau and the Tian Shan Range, the Tarim
Basin is a key element of the Cenozoic Asian orogenic system. However, a comprehensive …

The Karoo basins of south-central Africa evolved during the first-order cycle of
supercontinent assembly and breakup of Pangea, under the influence of two distinct tectonic …

A complete Alpine cross section integrates numerous seismic reflection and refraction
profiles, across and along strike, with published and new field data. The deepest parts of the …

We present a new compilation of estimates of modern rates of mechanical and chemical
denudation for externally drained basins exceeding 5× 105 km2 in area. These estimates …

ABSTRACT The Longmen Shan Foreland Basin developed as a flexural foredeep during
the Late Triassic Indosinian orogeny, spanning the time period c. 227–206 Ma. The basin fill …

The post-flysch (Oligocene–Miocene) palaeogeographic evolution of the entire North Alpine
Foreland Basin (NAFB) between Savoy (France) and Lower Austria is presented in eight …

Three‐dimensional modeling that integrates fluvial sediment transport, crustal‐scale tectonic
deformation, and lithospheric flexural subsidence is carried out to simulate the landscape …

Sediment supply to continental basins is determined at first order by the rate at which source
areas are eroded. Factors govering the rate of denudation are investigated using data from …

In regions undergoing active tectonics, the coupling between the tectonic displacement field,
the overlying landscape and the redistribution of mass at the Earth's surface in the form of …