- Geological and Geochemical Analysis
- High-pressure geophysics and materials
- earthquake and tectonic studies
- Geochemistry and Geologic Mapping
- Methane Hydrates and Related Phenomena
- Seismic Imaging and Inversion Techniques
- Seismology and Earthquake Studies
- Hydrocarbon exploration and reservoir analysis
- Geotourism and Geoheritage Conservation
Institute of Geology and Geophysics
2023-2024
Chinese Academy of Sciences
2023-2024
University of Chinese Academy of Sciences
2023-2024
The Central Anatolian Plateau, featuring its volcanic provinces, is a significant transition zone that marks the abrupt shift from continental collision and compressional deformation in east to oceanic subduction extensional dynamics west. A comprehensive understanding of physical properties, including seismic attenuation within crust, can illuminate potential causes geodynamic processes related activity. Here, we analyse S-wave peak delay using data Continental Dynamics–Central...
Abstract The Anatolian Plateau, currently experiencing rapid uplift and westward escape, records both the termination of oceanic subduction conversion to continental collision. crustal response transition environment from eastern western Anatolia can be inferred by seismic velocity attenuation structures. With this study, we construct a broadband Lg‐wave model for Plateau use it constrain lateral crust heterogeneities linked transition. Crustal Lg links late Cenozoic magmatism with...
During hydraulic fracturing (HF) stimulation in unconventional reservoir development, seismic attenuation significantly affects high frequency microseismic data. Analyzing parameters, including scattering and absorption, provides valuable insights into properties changes that result from HF injections. These parameters were mapped 3D using the MuRAT (multi-resolution tomography) software with a dataset of approximately 32,000 events over two years Weiyuan shale gas field...
Colossal and devastating earthquakes are typically associated with the slip rupture of fault zones. Fault zone imaging is challenging yet crucial to understand structure behavior, consequently hazard assessment mitigation. Seismic attenuation provides constraints on that independent seismic velocity imaging. Here, we image S-wave total (Qs) western part North Anatolian Zone (NAFZ) using data recorded by DANA (Dense Array for Anatolia) array. The area interest divided into three distinct...