Duanxin Chen

ORCID: 0000-0003-4414-4236
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About
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Research Areas
  • Methane Hydrates and Related Phenomena
  • Geological and Geophysical Studies
  • Hydrocarbon exploration and reservoir analysis
  • Geological formations and processes
  • Geology and Paleoclimatology Research
  • Seismic Imaging and Inversion Techniques
  • Geological Studies and Exploration
  • Atmospheric and Environmental Gas Dynamics
  • Geological Modeling and Analysis
  • Isotope Analysis in Ecology
  • Arctic and Antarctic ice dynamics
  • Geochemistry and Elemental Analysis

Chinese Academy of Sciences
2011-2023

Institute of Oceanology
2011-2023

Qingdao National Laboratory for Marine Science and Technology
2016-2022

Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)
2021-2022

University of Chinese Academy of Sciences
2011-2013

After the end of spreading South China Sea(SCS),an important structural movement-the Dongsha Movement took place at Northern Margin SCS.However,timing,range and dynamic mechanism is still unclear.Based on 2D/3D seismic data in area its neighboring,the mainly occurred late period Late Miocene ended Mio/ Pliocene boundary(5.5Ma) this paper.The affects Rise Chaoshan Depression.Besides,the eastern part Panyu Low-High southern northeastern Zhu Ⅰ Depression are also deformed.Its main deformation...

10.6038/j.issn.1004-2903.2012.03.022 article EN Progress in geophysics 2012-06-20

A new 3D seismic reflection data volume acquired in 2012 has allowed for the detailed mapping and characterization of gas hydrate distribution Pearl River Mouth Basin South China Sea. Previous studies core logging showed that occurrence at high concentrations is controlled by presence relatively coarse-grained sediment upward migration thermogenic from deeper section into overlying stability zone (BGHSZ); however, spatial remains poorly defined. We used a constrained sparse spike inversion...

10.1190/int-2015-0020.1 article EN Interpretation 2015-09-01

Gas hydrate dissociation may pose serious geohazards. The response of the seafloor to is important for geohazards, marine environments and global climate. We studied how affects underground temperature pressure lead deformation. Here, we designed a laboratory model experiment visualize fluid migration deformation during at atmospheric pressure. Our experiments show visible gas pipes, migratory pockets due explain newly discovered discordance between slide plane base stability zone. found...

10.1016/j.egyr.2021.08.187 article EN cc-by-nc-nd Energy Reports 2021-09-13

Abstract Fluid seepage sometimes impacts occurrences of submarine landslides, but the role landslide deposits in fluid is often neglected. Bathymetric data show that more than 1,000 seabed mounds are scattered over an elongated area at shelf edge northwestern South China Sea. Vertical seismic pipes subsurface spatially correlated with both surface and buried deposits. Detailed analyses within three‐dimensional (3D) survey least 221 231 (∼96%) have spatial correlation top edges multiple...

10.1029/2021gl096584 article EN Geophysical Research Letters 2022-03-03

Polygonal faults were identified from three-dimensional (3D) seismic data in the middle-late Miocene marine sequences of South China Sea. study area are normal with fault lengths ranging 100 to 1500 m, spaces 40 800 and throws 10 m. Gas hydrate was inferred polarity, reflection strength, temperature-pressure equilibrium computation results. hydrates located sediments above polygonal layer. can act as pathways for migration fluid flow, which supply hydrocarbons formation gas hydrates.

10.1155/2011/384785 article EN cc-by Journal of Geological Research 2011-12-05

Sedimentary organic matter (SOM) on continental slopes in marine regions can sensitively record climatic and environmental changes. In this study, total carbon content (TOC), nitrogen (TN), their stable isotope compositions (δ 13 C δ 15 N) for sediments of core G02 were investigated (at ∼24.2-year resolution) to reveal the temporal variations sources main controls distribution buried northwestern slope South China Sea over last ∼8600 years. Results a binary mixing model that ∼82.3 ± 3% SOM...

10.3389/feart.2023.1238920 article EN cc-by Frontiers in Earth Science 2023-08-17

The South China Sea is the biggest marginal sea in West Pacific.The environmental conditions are favorable there to growth of reefs.The Dongsha uplift was a shallow water area far from provenance Miocene.The marine including temperature,salinity and depth were excellent for reef growth.Base on integrated study seismic,well logging core data,and taking into account relative level changes,we believe that plenty reefs developed different horizons area,due complicated cooperation change regional...

10.3724/sp.j.1140.2012.01043 article EN Marine Geology & Quaternary Geology 2012-11-23

The types, influencing factors and their evolutions of focused fluid flow systems in the northern South China Sea (SCS) are deeply studied based on high-resolution 3D 2D seismic data. These include mud volcanoes, diapirs, gas chimneys, pipes, polygonal faults tectonic faults. They influenced by both tectonism sedimentation. diapirs volcanoes may have relationship unidirectional evolution we can separate them from whether sediments involved or fluids erupt into seawater not. Finally, a...

10.6038/cjg20141217 article EN 2014-12-01

The complexity of carbonate deposition and diagenesis leads to the reservoir heterogeneity.The analysis intersections well logs in area Liuhua oil field on Dongsha massif suggest that velocity,density seismic acoustic impedance are most relevant physical parameters porosity.Based quantitative properties from 3d logging data,we summarized this paper heterogeneous characteristics reef platform,and described its properties,by using techniques inversion attributes analysis.The results show...

10.3724/sp.j.1140.2011.04105 article EN Marine Geology & Quaternary Geology 2011-09-23

10.5281/zenodo.5563210 article EN Zenodo (CERN European Organization for Nuclear Research) 2021-10-12
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