A5101652356- earthquake and tectonic studies
- Geology and Paleoclimatology Research
- Geological and Geochemical Analysis
- Hydrocarbon exploration and reservoir analysis
- Geological and Geophysical Studies
- Geological formations and processes
- Methane Hydrates and Related Phenomena
- Computational Fluid Dynamics and Aerodynamics
- Metallurgy and Material Forming
- Landslides and related hazards
- Geoscience and Mining Technology
- Aerosol Filtration and Electrostatic Precipitation
- Inertial Sensor and Navigation
- Laser and Thermal Forming Techniques
- Metal Alloys Wear and Properties
- Dam Engineering and Safety
- Transportation Safety and Impact Analysis
- Electromagnetic Launch and Propulsion Technology
- HVDC Systems and Fault Protection
- Smart Grid and Power Systems
- Rock Mechanics and Modeling
- Hydropower, Displacement, Environmental Impact
- Technology-Enhanced Education Studies
- High-Voltage Power Transmission Systems
- Astronomical Observations and Instrumentation
Guangzhou Vocational College of Science and Technology
2024
Sun Yat-sen University
2019-2021
Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)
2020-2021
Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai)
2020-2021
Institute of Geology, China Earthquake Administration
2018-2021
China Earthquake Administration
2018-2021
Sinopec (China)
2014-2015
Electronic Navigation Research Institute
2014
Xi'an Jiaotong University
2014
China XD Group (China)
2012
Abstract The northwest striking Qishan‐Mazhao fault (QMF) accommodates complex deformation in the Tibet‐Ordos transition zone. We studied geologic and geomorphic expression of QMF using interpretations high‐resolution satellite images structure‐from‐motion models combined with detailed field investigations. Displaced loess tablelands, stream channels, fluvial terraces show that is predominately a left‐lateral strike‐slip minor normal component. magnetic susceptibility optically stimulated...
Abstract High‐resolution topographic data sets have now become increasingly available, which allows for remotely measuring and analyzing offset features their associated slip distributions at a very high resolution along fault, hence providing important insights into the fault behavior. The West Helanshan Fault is Holocene active right‐lateral strike‐slip located junction of Tibetan Plateau, Alashan, Ordos blocks. In this study, 2‐m‐resolution DEM was built from WorldView‐3 stereo satellite...
Abstract The Qilian Shan, located in the northeastern Tibet, is under strong tectonic activity and earthquake motion due to propagation of plateau. At mountain front eastern Tongziba River, southern Zhangye Basin, flows northward successively cuts Minle‐Damaying Fault Yonggu Anticline, two parallel structures within Frontal Thrust system Shan. Here we present a detailed record seven strath terraces this river that documents history active deformation structures. Based on estimated crustal...
<p indent="0mm">The Qaidam Basin is the largest Cenozoic basin located on northeastern margin of Tibetan Plateau. The extremely thick sedimentary strata in recorded regional tectonic deformation and associated climate change when Plateau grew outward to its margins. have been historically subdivided into seven primary stratigraphic units: Lulehe, Xia Ganchaigou, Shang Youshashan, Shizigou, Qigequan formations. Although many studies performed recent decades, Basin’s inception, development...
In view of the rapid development information technology, cultivation and promotion digital literacy higher vocational teachers has become an important issue in field education. The application deep learning soft computing technology provides strong technical support for this. This paper is to explore construction path evaluation model from perspective “AI+”. study deeply analyzes status quo teachers, focuses on combination potential intelligent algorithm based “AI+” perspective. research...
Ground deformation is usually used as direct evidence for early warning of geological hazards. The Weihe Graben, located in the southern margin Ordos Plateau, surrounded by many active faults. Earthquakes (e.g., 1556 Huaxian M 8 earthquake), mine accidents and ground fissures are major hazards that pose great threats to this densely populated region. In order characterise both tectonic anthropogenic activities we use Envisat data from 2003 2010 Sentinel-1 2014 2021, combined with levelling...
Abstract The Qilian–Haiyuan fault zone in the northeastern Tibetan Plateau has been source of strong earthquakes region. In its middle segment, Jinqianghe is an important active within Tianzhu seismic gap; however, little known about slip behavior. To present a new horizontal displacement distribution along this fault, we used WorldView‐2 stereo pairs and unmanned aerial vehicle‐based photogrammetry to construct digital elevation models obtain detailed tectono‐geomorphic interpretation...
Earthquake deformation is crucial for understanding fault kinematics. Modern earthquakes (moment magnitude <inline-formula xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink"> <tex-math notation="LaTeX">$M_{w} \geq 6$ </tex-math></inline-formula> ) have been well documented by geodetic techniques, such as radar interferometry and image correlation with unprecedented accuracy. Nonetheless, many large ( 7$ historical remain unexplored due to a lack of...
The deformation pattern and strain partitioning in the Eastern Chinese Tian Shan are poorly known because of lack quantitative study kinematics rate major structure. Here we report a late Quaternary shortening for most active reverse fault-and-fold Shan. We quantified Huoyanshan structure based on detailed high-resolution remote sensing image interpretations, field investigations geological mapping. Six generations folded terraces along Tuyugou valley that showed progressive folding process...
Abstract The Elashan fault (ELSF) and Qinghainanshan (QHNF), two major faults developed around the Qinghai Lake Chaka-Gonghe basins, are of great importance for investigating deformation model internal northeastern Tibetan Plateau. However, their late Pleistocene slip rates remain poorly constrained. In this study, we combine high-resolution topography acquired from unmanned aerial vehicles (UAV) geomorphological dating to calculate faults. We visited central ELSF western QHNF measured...
Abstract The deformation pattern and slip partitioning related to oblique underthrusting of the Tarim Basin in eastern Tian Shan orogenic belt are not well understood because interior images lacking. Baoertu fault is an E-W–striking, ~350-km-long reactivated basement structure within Shan. In this study, we quantify its late Quaternary activity based on interpretations detailed high-resolution remote sensing field investigations. Three observation sites along ~80-km-long segment indicate...
The Dongbatu Shan (DBTS, also known as the Nanjie Shan), which interrupts northern Tibetan foreland in Dunhuang basin, is an active anticline. It has accommodated northwestern growth of eastern Altyn Tagh fault system (ATF). Although several thrust faults have been identified around DBTS, their evolution history and influence on regional landscape received little attention during late-Quaternary. In this study, geomorphic methods are used to investigate interaction between drainage...
Earth and Space Science Open Archive This preprint has been submitted to is under consideration at Journal of Geophysical Research - Solid Earth. ESSOAr a venue for early communication or feedback before peer review. Data may be preliminary.Learn more about preprints preprintOpen AccessYou are viewing the latest version by default [v1]Late Quaternary active faulting on inherited Baoertu basement fault within eastern Tian Shan: Implications regional tectonic deformation slip partitioning, NW...