A5103405283- Geological and Geochemical Analysis
- earthquake and tectonic studies
- Geological and Geophysical Studies
- High-pressure geophysics and materials
- Geochemistry and Geologic Mapping
- Geochemistry and Elemental Analysis
- Hydrocarbon exploration and reservoir analysis
- Paleontology and Stratigraphy of Fossils
- Geological formations and processes
- Seismic Waves and Analysis
- Geology and Paleoclimatology Research
- Ocean Waves and Remote Sensing
- Geophysics and Gravity Measurements
- Oceanographic and Atmospheric Processes
- Geological Studies and Exploration
- Seismic Imaging and Inversion Techniques
- Remote Sensing and Land Use
- Landslides and related hazards
- Hydraulic Fracturing and Reservoir Analysis
- Earthquake Detection and Analysis
- Historical Astronomy and Related Studies
- Drilling and Well Engineering
- Aeolian processes and effects
- Coastal wetland ecosystem dynamics
- Seismic Performance and Analysis
Tarim University
2022-2023
Chengdu University of Technology
2008-2022
State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation
2008-2022
Research Institute of Petroleum Exploration and Development
2022
Guangzhou Institute of Geography
2019-2021
Guangdong Academy of Sciences
2021
Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)
2021
China Geological Survey
2017
University of Toronto
2015
Chinese Academy of Geological Sciences
2013-2014
The steep, high‐relief eastern margin of the Tibetan Plateau has undergone rapid Cenozoic cooling and denudation yet shows little evidence for large‐magnitude shortening or accommodation generation in foreland basin. We address this paradox by using a variety geomorphic observations to place constraints on kinematics slip rates several large faults that parallel plateau margin. Beichuan Pengguan are active, dominantly dextral‐slip structures can be traced continuously up 200 km along Both...
Widespread Cretaceous volcanic basins are common in eastern South China and crucial to understanding how the Circum-Pacific Tethyan plate boundaries evolved interacted with one another controlling tectonic evolution of China. Lithostratigraphic units these grouped, ascending order, into Early suite (K1V), Yongkang Group (K1-2), Jinqu (K2). SHRIMP U-Pb zircon geochronological results indicate that (1) (K1V) erupted at 136–129 Ma, (2) (K1-2) was deposited from 129 Ma 91 (3) deposition (K2)...
Abstract Fifteen sandstone samples taken from pre-Cretaceous strata of the Yangtze Block are analysed to constrain evolution South China Block, especially assembly between and Cathaysia blocks. The results show that maximum depositional age Neoproterozoic Lengjiaxi Group adjacent is c . 830 Ma, differing Kunyang Dahongshan groups (> 960 Ma) on southwestern margin Block. detrital zircons Palaeozoic have similar populations those in they may originate according palaeogeographic,...
Abstract The Sichuan Basin and the Songpan‐Ganze terrane, separated by Longmen Shan fold‐and‐thrust belt (the eastern margin of Tibetan Plateau), are two main Triassic depositional centres, south Qinling‐Dabie orogen. During Middle–Late closure Paleo‐Tethys Ocean, region, located at western Yangtze Block, transitioned from a passive continental into foreland basin. In meantime, Songpan‐Granze terrane evolved marine turbidite basin belt. To understand if how regional sediment routing system...
Based on analysis of field survey, drilling and seismic data, the formation evolution process Deyang–Anyue erosion rift trough in Sichuan Basin was reconstructed, exploration areas were divided evaluated. The results show that: (1) Dengying Formation around varies widely sedimentary characteristics. northern part developed deep-water sediments, basin varied gradually from to slope, platform margin, restricted platform, middle southern parts carbonate facies. (2) is formed by extensional...
Abstract A thrust‐fold belt consisting of a series thrusts and buckling folds developed in the Mesozoic Cenozoic strata within Kuqa Depression, Tarim Basin. In this study, structural interpretation model Depression is established proto‐basin reconstructed on basis outcrop geology along basin margin, seismic, well‐log CEMP data. The called ‘delaminate contractional deformation’, which emphasizes decoupling between Cenozoic, Mesozoic, pre‐Mesozoic basin‐basement but there no unified...
The Ordovician fracture-vug carbonate reservoirs of Tarim Basin, are featured by developed vugs, caves and fractures. strong heterogeneity results in huge uncertainty when these quantitatively characterized using merely static seismic data. effective quantitative characterization the has been an urgent problem to be solved. This study creatively proposes "second characterization" technique with combination dynamic data based on primary fully considering lots key influence factors conducting...
Abstract Five trenches across the Bootheel lineament, a possible surface expression of one coseismic faults great New Madrid earthquakes 1811 and 1812, indicate that ground failure took place along this 135-km-long feature, probably in or 1812. The morphology en echelon pattern north-northeast-trending lineament are suggestive strike-slip displacement on fault. Three cross portions which liquefied sand was injected. Vertically displaced strata were observed two these trenches, but could be...
Longmen Shan is located the special joint between Qinghai-Tibetan Plateau in west and Yangtze craton east. Consisting of a series parallel imbricated thrust, it develops, from to east, Maoxian-Wenchuan, Yingxiu-Beichuan Pengxian-Guanxian faults. Wenchuan Ms 8.0 earthquake thrust with strike-slip type, surface ruptures are fault zone Peng- xian-Guanxian zone. Based on geological background, tectonic setting, active tectonics Long- men earthquake, dynamical model illustrate possible links...
During the M s 8.0 Wenchuan Earthquake of May 12, 2008, three distinct faults in Longmen Shan along eastern margin Tibetan Plateau ruptured. We have carried out detailed field geological mapping on these (the Yingxiu-Beichuan, Pengxian-Guanxian, and Xiaoyudong Faults), as well minor Leigu Fault, using GPS total station surveys. The surface rupture consists two margin-parallel thrust linked by tear fault. By comparing features faults, spatial relationships between different ruptures can be...
After processing 204 data of historical earthquakes for M ⩾ 4.5 from 1900 to 1996 in the area centered at Beijing (39.9°N, 116.4° E; ±3°), two correlations have been suggested: One is between earthquake and position distribution major solar system bodies; other magnitude tidal force epicenter. A tentative presented future seism prediction. Because this work test stage based on a statistic analysis, further verification are expected.