A5101783226- Methane Hydrates and Related Phenomena
- Geology and Paleoclimatology Research
- Geological and Geophysical Studies
- Hydrocarbon exploration and reservoir analysis
- Paleontology and Stratigraphy of Fossils
- Geochemistry and Elemental Analysis
- Geological and Geochemical Analysis
- Geological formations and processes
- Coral and Marine Ecosystems Studies
- Heavy metals in environment
- Isotope Analysis in Ecology
- Atmospheric and Environmental Gas Dynamics
- earthquake and tectonic studies
- Marine and coastal ecosystems
- Underwater Acoustics Research
- Mercury impact and mitigation studies
- Tree-ring climate responses
- High-pressure geophysics and materials
- Plant Water Relations and Carbon Dynamics
- Marine and fisheries research
- Environmental Quality and Pollution
- Marine animal studies overview
- Environmental Education and Sustainability
- Ecology and Vegetation Dynamics Studies
- Oceanographic and Atmospheric Processes
Chinese Academy of Sciences
2015-2024
South China Sea Institute Of Oceanology
2015-2024
Institute of Oceanology
2015-2024
University of Chinese Academy of Sciences
2012-2024
Northwest A&F University
2024
Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)
2020-2023
Nanjing University
2023
Beijing Normal University
2018-2022
Research Center for Eco-Environmental Sciences
2022
Gansu Research Institute of Chemical Industry
2017
Abstract The tectonic evolution of the South China Sea is closely associated with multiple subduction-collision processes in Southeast Asia. When collision Dangerous Grounds terrane Sabah-Palawan Islands terminated debated due to poor age constraints at southern margin Sea. A deep well drilled on Meiji Atoll penetrates Cenozoic carbonate strata central Grounds. Robust strontium isotope ages and laser ablation–inductively coupled plasma–mass spectrometry (LA-ICP-MS) U-Pb dates provide...
Abstract Free gas migration through the hydrate stability zone (GHSZ) and subsequent seepage at seabed are characteristic features in marine provinces worldwide. The biogenic or thermogenic is typically transported along faults from deeper sediment strata to GHSZ. Several mechanisms have been proposed explain free transport While inhibition of formation by elevated salinities temperatures addressed previously studies simulating unfocused, area‐wide upward advection gas, which not adequately...
The response of radial growth to climate and the sensitivity tree at different ages in drought conditions are essential for predicting forest dynamics making correct management policies. In this study, we analyzed responsiveness Picea crassifolia Kom. explored relationship between age individual scale wetter eastern area drier western Qilian Mountains. Pearson correlation coefficients were calculated chronology each climatic factors examine climate-growth relationships. Linear fitting,...
The Baiyun deepwater region (Shenhu area) of the Pearl River Mouth Basin (PRMB), northern South China Sea (SCS), is characterized by presence abundant gas hydrate deposits and dense submarine canyons. However, relationships between decomposition formation canyons remain unclear. Based on seismic well data, variations stability zone (GHSZ) thickness were quantitatively calculated. results indicate that GSHZ, which ranges from 0 to 350m, distributed in areas where water depth exceeds 600m....
Many researchers have estimated the thickness of gas hydrate stability zone (GHSZ) and amount at different areas in South China Sea (SCS) using varying methods, but few reported calculations for whole SCS.In this paper, Milkov Sassen's model is used to calculate GHSZ addition, an estimation discussed terms composition effects water depth.Average thicknesses SCS are be ~440 m, ~477 m ~553 based on relationship between depth established study 3 kinds hydrates with containing 100% methane, 96%...