A5008288912- earthquake and tectonic studies
- High-pressure geophysics and materials
- Geological and Geochemical Analysis
- Seismic Imaging and Inversion Techniques
- Seismic Waves and Analysis
- Geological and Geophysical Studies
- Methane Hydrates and Related Phenomena
- Hydraulic Fracturing and Reservoir Analysis
- Geological formations and processes
- Geological Modeling and Analysis
- Seismology and Earthquake Studies
- Geology and Paleoclimatology Research
- Geophysical Methods and Applications
- Hydrocarbon exploration and reservoir analysis
- Geomagnetism and Paleomagnetism Studies
- Computer Graphics and Visualization Techniques
- Earthquake Detection and Analysis
- Geochemistry and Geochronology of Asian Mineral Deposits
- Reservoir Engineering and Simulation Methods
- Landslides and related hazards
- Semantic Web and Ontologies
- Geomechanics and Mining Engineering
- Geophysics and Sensor Technology
- Underwater Acoustics Research
- Drilling and Well Engineering
First Affiliated Hospital of Zhengzhou University
2025
Institute of Geology and Geophysics
2015-2024
Chinese Academy of Sciences
2015-2024
Huzhou University
2024
Mineral Resources
2024
University of Chinese Academy of Sciences
2024
Bohai University
2023
SEGi University
2023
Center for Excellence in Tibetan Plateau Earth Sciences
2015-2021
University of Illinois Urbana-Champaign
2019
Plenty of gold deposits related to Late Mesozoic craton destruction are widely distributed in eastern North China Craton. However, significant differences research degrees, ore-forming characteristics, and proven reserves exist among different regions the The Liaodong Peninsula has similar regional geological characteristics those Jiaodong Peninsula, with both experiencing during Mesozoic, but two areas have substantial terms mineralization resources. Based on geology, magmatic-tectonic...
Abstract The left‐lateral Altyn Tagh Fault (ATF) system is the northern boundary of Tibetan Plateau resulted from India–Eurasia continental collision. How intracontinental deformation across central ATF responds to distal collision remains elusive, primarily due unclear crustal structure. We obtained detailed structure using receiver functions recorded by ∼NW–SE oriented linear dense array. images reveal Tarim lower crust underthrusting beneath and reaches a maximum depth ∼75 km undergoing...
1848 specimens were collected systematically from about 900 horizons in the loess profile of Xifeng, Gansu province, China. The magnetostratigraphy is established on basis palaeomagnetic results after thermal cleaning, usually at 300°C. This result has been found to be generally consistent with previous work Luochuan. susceptibility varies regularly appearance and palaeosol thus could used as a criterion classify sequence.
West–east extension is a prominent tectonic feature of southern and central Tibet despite ongoing north–south (N–S) convergence between India Eurasia. Knowledge deep structure beneath the N–S trending rifts key to evaluating models proposed for their origin, including gravitational collapse, oblique along arcuate plate boundary, mantle upwelling. We model direct S Moho-reflected SsPmp phases at teleseismic distances constrain variations in crustal thickness across major crossed by ∼900-km...
In full waveform inversion (FWI) with the least-squares (L2) norm, direct amplitude matching is never perfect and accurate estimation of seismic source strength not always available. contrast, normalized zero-lag cross-correlation objective function relaxes on constraints emphasizes phase information when measuring closeness between simulated observed data. This FWI method becomes insensitive to differences in amplitude. Based this property, we investigate effectiveness robustness (CFWI)...
Measurements of specimens from the loess profile Xifeng, Gansu province, China, all show original magnetic fabric for sediments, i.e. nearly horizontal foliation and commonly oblate magnitude ellipsoid. The degree anisotropy always shows a strong correlation with F rather than lineation L. Specimens wind-blown loess, redeposited water-lain red clay their own distribution areas respectively in diagram L versus F. Magnetic provides evidence suggestion that clay, like overlying is aeolian...
Recently constructed models of crustal structure across Tibet based on surface wave data display a prominent mid-crustal low velocity zone (LVZ) but are vertically smooth in the crust. Using six months broad-band seismic recorded at 22 stations arrayed approximately linearly over 440 km observation profile northeastern (from Songpan–Ganzi block, through Qaidam into Qilian block), we perform Bayesian Monte Carlo joint inversion receiver function with dispersion to address whether layering is...