The Pamir Frontal Thrust along the leading edge of the northern Pamir is characterized by multiple earthquakes with moment magnitudes of 6.5–...

Bending‐moment faults and flexural‐slip faults (FSFs), as two basic fault styles due to bending‐related tangential longitudinal s...

Fluvial planation surfaces, such as straths, commonly serve as recorders of climatic and tectonic changes and are formed by the lateral erosion of ...

The Pamir‐Tian Shan collision zone in the western Tarim Basin, northwest China, formed from rapid and ongoing convergence in response to the ...

Understanding the evolution of continental deformation zones relies on quantifying spatial and temporal changes in deformation rates of tectonic st...

Flexural slip plays an important role in accommodating fold growth, and its topographic expression, flexural‐slip fault (FSF) scarps, may be ...

Streams commonly respond to base‐level fall by localizing erosion within steepened, convex knickzone reaches. Localized incision causes knick...