The conventional view of crustal deformation in the reactivated Tianshan orogenic belt is
strong north–south (NS) compression accommodated by a series of east–west (E–W) …

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

The Tianshan orogenic belt, part of the Central Asian Orogenic Belt, offers an opportunity to
examine the complexities of an orogenic system that records long‐term intracontinental …

Abstract The Eastern Tianshan and East Junggar orogenic belts are major constituents of
the southwestern Central Asian Orogenic Belt. This study applies low-temperature …

Thermochronological datasets for the Kyrgyz Tianshan and Siberian Altai-Sayan within
Central Asia reveal a punctuated exhumation history during the Meso–Cenozoic. In this …

Abstract In Central Asia, numerous fragments of planation surfaces are visible within the
present day topography. However, their precise timing of formations is still poorly …

Abstract The Junggar‐Balkhash Ocean was a major branch of the southern Paleo‐Asian
Ocean. The timing of its closure is important for understanding the history of the Central …

Abstract The Uzbek Tian Shan is a prominent metal-rich belt, hosting world-class orogenic
Au deposits such as Muruntau. However, its post-collisional history in relation to fluid …

The Tianshan belt forms the southwestern part of the Central Asian Orogenic Belt, and its
current topography is a product of punctuated Meso-Cenozoic intra-continental deformation …

Abstract The western Chinese Tianshan, located in the southern domain of the Central
Asian Orogenic Belt (CAOB), was originally established by multiple accretion-collision …