A5006394124- Geological and Geochemical Analysis
- earthquake and tectonic studies
- Geology and Paleoclimatology Research
- Geological and Geophysical Studies
- High-pressure geophysics and materials
- Geochemistry and Geologic Mapping
- Geological formations and processes
- Geochemistry and Elemental Analysis
- Landslides and related hazards
- Geochemistry and Geochronology of Asian Mineral Deposits
- Aeolian processes and effects
- Plant Diversity and Evolution
- Geological Studies and Exploration
- Hydrocarbon exploration and reservoir analysis
- Paleontology and Stratigraphy of Fossils
- Nanoparticle-Based Drug Delivery
- Nanoplatforms for cancer theranostics
- Facial Rejuvenation and Surgery Techniques
- Hydrology and Sediment Transport Processes
- Membrane Separation Technologies
- Advanced ceramic materials synthesis
- Pleistocene-Era Hominins and Archaeology
- Advanced Nanomaterials in Catalysis
- Heavy metals in environment
- Advanced materials and composites
China University of Geosciences
2014-2025
Shanghai Jiao Tong University
2023
State Key Laboratory of Geological Processes and Mineral Resources
2020
Beihang University
2018
University of Illinois Urbana-Champaign
1989
Abstract The pattern and timing of deformation in southeast Tibet resulting from the early stages India-Asia collision are crucial factors to understand growth Tibetan Plateau, but they remain poorly constrained. Detailed field mapping, structural analysis, geochronological thermochronological data along a 120 km section Ludian-Zhonghejiang fold-and-thrust belt bounding Jianchuan basin western Yunnan, China, document Cenozoic tectonic evolution conjunction between Lanping-Simao South China...
Wind is one of the most dominant agents erosion and dust production in arid basins within continental interior central Asia. However, interactions between water wind landscape evolution stony deserts remain unclear. We present an integrated geomorphologic, sedimentologic, chronologic study from Hami Basin propose a hypothesis on that may apply to other East Asian deserts. precipitation-driven contributed lowering basin floor emissions. A 10Be depth profile isolated terrace (TN3) yields...
This study explores the formation, preservation, and uplift of relict low-relief surfaces in Barkol Mountains, coupled with sedimentological geochemical insights from Hami Basin. By integrating digital geomorphic analysis, structural mapping, thermochronology, sedimentary data, research reconstructs tectonic evolution this region.Using Shuttle Radar Topography Mission (SRTM) data (3-arc-second resolution), Mountains were identified based on slope thresholds (
Abstract The Gyirong basin, southern Tibet, contains the record of Miocene‐Pliocene exhumation, drainage development, and sedimentation along northern flank Himalaya. tectonic controls on basin formation their potential link to South Tibetan Detachment System (STDS) are not well understood. We use detrital zircon (ZFT) apatite (AFT) fission‐track analysis, together with U‐Pb dating decipher provenance sediments exhumation history source areas. Results presented for nine samples (AFT, ZFT,...
Abstract The Jiacha Gorge in southeastern Tibet is the second-largest deeply incised gorge of Yarlung-Tsangpo River, after Tsangpo Gorge. A late Cenozoic N-S–trending normal fault, Woka Rift coincides with western limit gorge. However, relationship between formation gorge, drainage evolution, and rift activity remains unclear. Analysis river long profile suggests that developed as a ~45-km-wide knickzone, rather than local knickpoint. Projection tributary stream profiles indicate...
The West Junggar orogen, located in the southwestern Central Asian Orogenic Belt (CAOB), preserves an abundant record of tectonic processes associated with evolution Ocean. In this study, we use detrital zircon U–Pb age data from Ordovician to Carboniferous sandstones southern and central domains, complemented by literature data, better constrain CAOB. Kekeshayi, Qiargaye, Laba formations domain were deposited during Darriwilian-Sandbian, Katian-Aeronian, Homerian-Emsian, respectively....
Abstract Analysing the provenance changes of synorogenic sediments in Turpan‐Hami basin by detrital zircon geochronology is an efficient tool to examine uplift and erosion history easternmost Tian Shan. We present U‐Pb analysis from nine samples that were collected within marginal lacustrine Middle‐Late Jurassic aeolian‐fluvial Early Cretaceous strata basin. Middle‐Early (159–172 Ma) zircons deriving southern Junggar dominated Middle sample western basin, whereas Permian‐Carboniferous...
Abstract Wind is one of the major processes modifying land surface in Hami Basin, as evidenced by wind deflation gravel lags, yardangs, and mantled eolian ripples. We report erosion rates for Basin using cosmogenic 10 Be measurements. Bedrock average 0.121 ± 0.0293 mm yr −1 , which similar to those other wind‐eroded arid basins East Asia, but anomalously low when modern near‐surface speeds are considered. posit that interglacial periods experienced lower than glacial periods, was likely once...
The India-Asia collision reactivated the early Paleozoic Qilian orogen with an intense metamorphic belt that promoted release of metamorphism-generated radiogenic Sr into drainage systems on NE Tibetan Plateau. This impact regional dissolved cycle is well observed at recent−modern scale, but its onset and evolutionary histories are unclear. We present first basin-scale 52−5 Ma isotopic record in water Plateau by analyzing well-dated basin fluvial-lacustrine sediments Xining, Linxia, Tianshui...
Cretaceous eolian deposits provide evidence of variations in the tropical-subtropical atmospheric circulation under greenhouse conditions. However, misinterpretation many such as fluvial or deltaic originally hindered precise paleoclimatic reconstructions. Here we report a newly identified Early desert Hami Basin, China, which helps understand spatial-temporal aridity and circulations within central East Asia during Cretaceous. The Liushuquan Formation is composed >300-m-thick...