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 Tianshan range, located in the southern Central Asian Orogenic Belt (CAOB),
represents an excellent natural laboratory for investigating intracontinental deformation. The …

Geothermochronologic data outline the temperature‐deformation‐time evolution of the
Muskol and Shatput gneiss domes and their hanging walls in the Central Pamir. Prograde …

The Pamirs represent the indented westward continuation of the northern margin of the
Tibetan Plateau, dividing the Tarim and Tajik basins. Their evolution may be a key factor …

The northward indentation of the Pamir salient into the Tarim basin at the western syntaxis of
the India‐Asia collision zone is the focus of controversial models linking lithospheric to …

This study provides new low-temperature thermochronometric data, mainly apatite fission
track data on the basement rocks in and adjacent to the Talas-Fergana Fault, in the Kyrgyz …

Abstract Along the Ghissar‐Alai Range of the southwestern Tian Shan (southwestern
Kyrgyzstan, northern Tajikistan), the deformation front of the India‐Asia collision—the Pamir …

Abstract The Junggar Alatau forms the northern extent of the Tian Shan within the Central
Asian Orogenic Belt (CAOB) at the border of SE Kazakhstan and NW China. This study …

Abstract The dextral Talas‐Fergana Fault separates the western from the central Tien Shan.
Recent work has shed light on the Cenozoic evolution of the eastern and central Tien Shan; …

Central Asia hosts the most extensive and highest topography on Earth, which is the result of
the feedbacks among rock uplift, atmospheric circulation and moisture transport, and …