Area of research
Geophysics · Artificial Intelligence
Research interest
Research interests include Geological and Geochemical Analysis, High-pressure geophysics and materials, earthquake and tectonic studies, and Geochemistry and Geologic Mapping.
Deep learning-based detection of primary bone tumors around the knee joint on radiographs: a multicenter study
Large-scale rare-metal pegmatite deposit formation driven by supercontinent assembly
Tibetan Plateau insights into >1100 °C crustal melting in the Quaternary
Jurassic Paleomagnetism of the Lhasa Terrane—Implications for Tethys Evolution and True Polar Wander
Post-Collisional Silica-Undersaturated Bamaoqiongzong Volcanic Rocks from Northern Qiangtang: Indicators of the Mantle Heterogeneity and Geodynamic Evolution of Central Tibet
Short duration of Early Permian Qiangtang-Panjal large igneous province: Implications for origin of the Neo-Tethys Ocean
Passive-margin magmatism caused by enhanced slab-pull forces in central Tibet
Pliocene-Quaternary crustal melting in central and northern Tibet and insights into crustal flow
Andesitic crustal growth via mélange partial melting: Evidence from Early Cretaceous arc dioritic/andesitic rocks in southern Qiangtang, central Tibet
Underplating of basaltic magmas and crustal growth in a continental arc: Evidence from Late Mesozoic intermediate–felsic intrusive rocks in southern Qiangtang, central Tibet
Phanerozoic amalgamation of the Alxa Block and North China Craton: Evidence from Paleozoic granitoids, U–Pb geochronology and Sr–Nd–Pb–Hf–O isotope geochemistry
Overlapping Sr–Nd–Hf–O isotopic compositions in Permian mafic enclaves and host granitoids in Alxa Block, NW China: Evidence for crust–mantle interaction and implications for the generation of silicic igneous provinces
Petrogenesis of a Late Carboniferous mafic dike–granitoid association in the western Tianshan: Response to the geodynamics of oceanic subduction
Paleoproterozoic S-type granites in the Helanshan Complex, Khondalite Belt, North China Craton: Implications for rapid sediment recycling during slab break-off