A5060827715- Geological and Geophysical Studies
- Methane Hydrates and Related Phenomena
- Geological formations and processes
- earthquake and tectonic studies
- Hydrocarbon exploration and reservoir analysis
- Geological and Geochemical Analysis
- Geological Studies and Exploration
- Seismic Imaging and Inversion Techniques
- Geology and Paleoclimatology Research
- Geophysics and Gravity Measurements
- Isotope Analysis in Ecology
- Marine and coastal ecosystems
- Paleontology and Stratigraphy of Fossils
- High-pressure geophysics and materials
- Surface Treatment and Coatings
- Electrochemical sensors and biosensors
- Asian Culture and Media Studies
- Magnesium Alloys: Properties and Applications
- Gender, Feminism, and Media
- Geochemistry and Elemental Analysis
- Advanced biosensing and bioanalysis techniques
- Geochemistry and Geochronology of Asian Mineral Deposits
- Seismic Waves and Analysis
- High-Voltage Power Transmission Systems
- High Entropy Alloys Studies
Guangzhou Marine Geological Survey
2016-2025
Ministry of Natural Resources
2022-2025
China Geological Survey
2016-2025
Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)
2021-2024
Columbia University
2024
Jiangsu University
2014
Institute of Oceanology
2004-2011
Tebian Electric Apparatus (China)
2011
South China Sea Institute Of Oceanology
2011
Central South University
2011
Abstract Combined analyses of deep tow magnetic anomalies and International Ocean Discovery Program Expedition 349 cores show that initial seafloor spreading started around 33 Ma in the northeastern South China Sea (SCS), but varied slightly by 1–2 Myr along northern continent‐ocean boundary (COB). A southward ridge jump ∼20 km occurred 23.6 East Subbasin; this timing also was coeval to onset Southwest Subbasin, which propagated for about 400 southwestward from ∼23.6 ∼21.5 Ma. The terminal...
Abstract Coring/logging data and physical property measurements from International Ocean Discovery Program Expedition 349 are integrated with, correlated to, reflection seismic to map sequence boundaries facies of the central basin neighboring regions South China Sea. First‐order interpreted, which Oligocene/Miocene, middle Miocene/late Miocene, Miocene/Pliocene, Pliocene/Pleistocene boundaries. A characteristic early Pleistocene strong reflector is also identified, marks top extensive...
The development of the Mesozoic proto−South China Sea was closely related to tectonic evolution Tethys and Paleo-Pacific domains may have been a key driving mechanism for opening South Sea. Despite its importance, direct geologic evidence remains limited, is debated between two primary models: intra-oceanic subduction oceanic-continental subduction. Here, we present petrographic, geochronologic, geochemical data from tuffs Eocene−Pliocene sedimentary records in Sabah, northern Borneo....
During the Mesozoic, Southeast (SE) Asia (including South China and Sea (SCS)) was located in a transitional area between Tethyan Pacific geotectonic regimes. However, it is unclear whether geodynamic processes SE Asian continental margin were controlled by or paleo-Pacific Ocean subduction. Herein, we report ~124 Ma adakitic granodiorites Nb-enriched basalts from Xiaozhenzhu Seamount of SCS. Granodiorites have relatively high Sr/Y (34.7–37.0) (La/Yb)N (13.8–15.7) ratios, as well low Y...
Mud volcanoes are important to understand hydrocarbon research and exploration, crustal movement neotectonic activity, geological engineering, climate change. They widely distributed along the Alps‐Tethys suture zone, Pacific belt, continental slopes. Previous detailed studies on mud concentrated mostly onshore areas. Recent developments in geophysical technology have opened vast deepwater areas for volcanoes. Based multibeam bathymetry, multichannel seismic reflection, gravity, magnetics...
The Zhongjiannan Basin is located west of the South China Sea (SCS) and was affected by left-lateral strike-slip Red River Fault (RRF), West Edge (WEFSCS) continental rifting in early Cenozoic. formed a strike-pull basin with an S‒N distribution. During middle Miocene, sea spreading SCS stopped, but dynamic mechanism Basin, which controlled sedimentary structural evolution after late remains unclear. In this paper, through segment interpretation latest seismic section we conduct comparative...
Porous composite titania photocatalytic films were fixed on steel substrate by plasma electrolytic oxidation. Aluminate solution containing TiO 2 nanopowders was used as electrolyte. The microstructure and activities of the studied. investigation results revealed that when electrolyte contained a few powders, film consisted A-TiO , Al 5 γ-Al O 3 . With increasing concentration powders in electrolyte, phase disappeared, surface content Ti element increased. coarse porous, which became more...