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  1.  24
    Characterization of Gas Hydrate Distribution Using Conventional 3D Seismic Data in the Pearl River Mouth Basin, South China Sea.Xiujuan Wang, Jin Qian, Timothy S. Collett, Hesheng Shi, Shengxiong Yang, Chengzhi Yan, Yuanping Li, Zhenzhen Wang & Duanxin Chen - 2016 - Interpretation: SEG 4 (1):SA25-SA37.
    A new 3D seismic reflection data volume acquired in 2012 has allowed for the detailed mapping and characterization of gas hydrate distribution in the Pearl River Mouth Basin in the South China Sea. Previous studies of core and logging data showed that gas hydrate occurrence at high concentrations is controlled by the presence of relatively coarse-grained sediment and the upward migration of thermogenic gas from the deeper sediment section into the overlying gas hydrate stability zone ; however, the spatial distribution (...)
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  2.  19
    Characterization of Hydrate-Bearing Sediments Recovered From the Shenhu Area of the South China Sea.Changling Liu, Qingguo Meng, Gaowei Hu, Chengfeng Li, Jianye Sun, Xingliang He, Nengyou Wu, Shengxiong Yang & Jinqiang Liang - 2017 - Interpretation: SEG 5 (3):SM13-SM23.
    The characteristics of the hydrate-bearing layer are important parameters for gas hydrate exploration and exploitation, which can be provided by laboratory analysis. We have carried out a systematic analysis of modern instruments, including the laser grain size analyzer, X-ray computed tomography, scanning electron microscopy, X-ray diffraction, Raman spectroscopy, gas chromatography, and isotope mass spectrometry, on the hydrate-bearing sediment samples recovered from the Shenhu area in the South China Sea in 2016. We focused on the structure, hydration number, and gas composition (...)
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  3.  26
    Characterization of Hydrate-Bearing Sediments Recovered From the Shenhu Area of the South China Sea.Changling Liu, Qingguo Meng, Gaowei Hu, Chengfeng Li, Jinaye Sun, Xingliang He, Nengyou Wu, Shengxiong Yang & Jinqiang Liang - forthcoming - Interpretation: SEG:1-39.
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  4.  15
    Evaluation of Gas Hydrate-Bearing Sediments Below the Conventional Bottom-Simulating Reflection on the Northern Slope of the South China Sea.Jinqiang Liang, Zijian Zhang, Pibo Su, Zhibin Sha & Shengxiong Yang - 2017 - Interpretation: SEG 5 (3):SM61-SM74.
    The continuous bottom-simulating reflection is commonly considered to mark the base of gas hydrate stability zone. Below this depth, gas hydrate gives away to free gas or water filling with pore spaces of sediments. We integrated and analyzed seismic data collected in 2008, and logging-while-drilling data and coring results acquired by the Fugro Voyager in 2015 in the Shenhu area on the northern slope of the South China Sea. Based on seismic and well-log correlation, a BSR with typical characteristics of (...)
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  5.  19
    Introduction to Special Section: Gas Hydrates in the South China Sea.Guangfa Zhong, Hongliu Zeng, Shengxiong Yang, Jinqiang Liang, Xuewei Liu, Xin Su, Xiujuan Wang, Changling Liu & Ming Su - 2017 - Interpretation: SEG 5 (3):SMi-SMi.
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  6.  7
    Introduction to Special Section: The South China Sea Deep-Water: Stratigraphy, Sedimentology, and Resources.Guangfa Zhong, Hongliu Zeng, Shiguo Wu, Char-Shine Liu, Weilin Zhu, Shengxiong Yang, Xinong Xie & Haibin Song - 2016 - Interpretation: SEG 4 (3):SPi-SPi.
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