The source-to-sink fluctuations of Asian aeolian deposits have been investigated over the
past two decades using multiple mineralogical and geochemical tracers. These source …

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

Eastward transport and clockwise rotation of crust around the southeastern margin of the
Tibetan Plateau dominates active deformation east of the Eastern Himalayan Syntaxis …

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 …

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

New low‐temperature thermochronological data from 80 samples in eastern Kyrgyzstan are
combined with previously published data from 61 samples to constrain exhumation in a …

Abstract During the Late Palaeozoic–Mesozoic, Central Asia and Tibet were affected by
several geodynamic episodes that induced either large-scale compression or widespread …

The collision of India with Eurasia has caused rejuvenated deformation and uplift of the
remote Tian Shan intracontinental orogenic range and has led to deposition of thick …

As a typical intracontinental orogenic belt, the Tian Shan range is a natural lab for the
understanding of ongoing intraplate deformation and related geodynamic mechanisms …

Cenozoic exhumation in the Tianshan is controlled by a complex interaction between
tectonics and climate. However, the timing and magnitude of exhumation of the Tianshan …