Elevated gas hydrate saturation within silt and silty clay sediments in the Shenhu area, South China Sea

[1] Gas hydrate saturations were estimated using five different methods in silt and silty clay foraminiferous sediments from drill hole SH2 in the South China Sea. Gas hydrate saturations derived from observed pore water chloride values in core samples range from 10 to 45% of the pore space at 190–2... View More