The India–Asia collision zone is a key area for understanding continental plateau formation
and mountain building. Two fundamental questions in this context are how the …

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 …

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 …

Earthquake scarps associated with recent historical events have been found on the floor of
the Sea of Marmara, along the North Anatolian Fault (NAF). The MARMARASCARPS cruise …

Abstract The 2008 M w 7.9 Wenchuan earthquake ruptured an imbricate thrust system in the
Longmen Shan range, which forms the eastern boundary of the Tibetan Plateau. We use …

In the last decades surface exposure dating using cosmogenic nuclides has emerged as a
powerful tool in Quaternary geochronology and landscape evolution studies. Cosmogenic …

The dating of the uplift onset of the Mongolian mountain ranges, the northernmost relief
associated with the India-Eurasia convergence, is a fundamental issue to better understand …

Millennial slip rates have been determined for the Altyn Tagh fault (ATF) at three sites near
Aksay (∼ 94° E) in northeastern Tibet by dating fluvial channels and terrace riser offsets with …

We determined vertical components of slip rates of 0.22±0.03 mm a− 1 for the Jiayuguan
fault and 0.11±0.03 mm a− 1 for the Jintanan Shan fault, which lie along the northeastern …

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 …