In one form or another, geochronologists have been practicing thermochronology1, the use
of radioisotopic dating to constrain thermal histories of rocks and minerals, for over 40 years …

Research in landscape evolution over millions to tens of millions of years slowed
considerably in the mid‐20th century, when Davisian and other approaches to …

In the last decade apatite (U–Th)/He thermochronometry has emerged as an important tool
for quantifying the cooling history of rocks as they pass through the upper 1–3 km of the …

Recent data on He diffusion challenge the temperature sensitivity of apatite (U–Th)/He
thermochronology: the damage induced by recoil of U and Th decay series during emission …

The present‐day topography of the Tian Shan range is considered to result from crustal
shortening related to the ongoing India‐Asia collision that started in the early Tertiary. In this …

Many thermochronology studies focus on extracting the thermal history of a sample using
fission-track length distributions and track annealing models (eg, Ketcham 2005, and …

Extension and associated tectonic exhumation have been described across a diverse
spectrum of geodynamic environments, ranging from lithospheric-scale extension along …

Some of the lowest weathering and erosion rates in any mountain range in the world have
been measured using cosmogenic nuclides in the steep, humid, tropical highlands of Sri …

The equilibrium form of the fluvial long profile has been used to elucidate a wide range of
aspects of landscape history including tectonic activity in tectonic collision zones, and in …

Atlantic‐type continental margins have long been considered “passive” tectonic settings
throughout the entire postrift phase. Recent studies question the long‐term stability of these …