This paper presents a review of the Quaternary–Recent deformation field and mountain
building processes within the Gobi Corridor region of Central Asia, which includes the North …

Strike–slip faults are often accompanied by a variety of structures, particularly at their tips.
The zones of additional fracturing are classified as tip‐damage zones. These zones can be …

We use observations of surface faulting, well-constrained earthquake focal mechanisms and
centroid depths, and velocity structure determined by surface wave propagation and …

The Zagros mountains of SW Iran are one of the most seismically active intra-continental fold-
and-thrust belts on Earth, and an important element in the active tectonics of the Middle East …

Whether strike‐slip fault systems in Eurasia accomplish eastward extrusion of Tibetan crust
and lithosphere depends largely on the kinematics of deformation at the fault tip. Here we …

We present new geodetic results of crustal velocities over a large part of northern Asia
based on GPS measurements in the Baikal rift zone and Mongolia spanning the 1994–2002 …

We use archaeological evidence to identify ancient earthquakes in the vicinity of large 20th
century events in the Iranian Plateau. Two large earthquakes on the Zagros Main Recent …

Abstract In the western Great Basin of North America, a system of dextral faults
accommodates 15%–25% of the Pacific–North American plate motion. The northern Walker …

We use drainage reconstructions to estimate long-term offsets on the Gowk fault, an oblique
right-lateral strike-slip fault in eastern Iran, on which there have been a number of recent …

Mountain ranges that are actively forming around the western and northern perimeter of the
Indo-Eurasia collisional deformational field, such as the Mongolian Altai, comprise a unique …