Re‐examination on The Contribution of Deep Thermogenic Gas to Shallow Hydrate in The Shenhu Area, Northern Continental Slope of South China Sea
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N. Wu | Pibo Su | X. Cong | Rui Yang | Shaohua Qiao
[1] Richard B. Coffin,et al. Deep Sediment-Sourced Methane Contribution to Shallow Sediment Organic Carbon: Atwater Valley, Texas-Louisiana Shelf, Gulf of Mexico , 2015 .
[2] Richard B. Coffin,et al. Contribution of Vertical Methane Flux to Shallow Sediment Carbon Pools across Porangahau Ridge, New Zealand , 2014 .
[3] S. Min. Structural Characteristics in the Shenhu Area,Northern Continental Slope of South China Sea,and Their Influences on Gas Hydrate , 2014 .
[4] Huang Xia,et al. Gas Sources of Natural Gas Hydrates in the Shenhu Drilling Area, South China Sea: Geochemical Evidence and Geological Analysis , 2013 .
[5] Lijun Mi,et al. Focused fluid flow in the Baiyun Sag, northern South China Sea: implications for the source of gas in hydrate reservoirs , 2013, Chinese Journal of Oceanology and Limnology.
[6] Qiao Shao-hu. Migration and Accumulation System: The Key Control Factors of Heterogeneous Distribution of Gas Hydrate , 2013 .
[7] Jinqiang Liang,et al. Gas Hydrate System of Shenhu Area, Northern South China Sea: Geochemical Results , 2011 .
[8] T. Pape,et al. Molecular and isotopic partitioning of low-molecular-weight hydrocarbons during migration and gas hydrate precipitation in deposits of a high-flux seepage site , 2010 .
[9] J. Chanton. The effect of gas transport on the isotope signature of methane in wetlands , 2005 .