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Geoscience ›› 2008, Vol. 22 ›› Issue (3): 376-381.

• Engineering Geology and Environmental Geology • Previous Articles     Next Articles

Micro-textures of Methane Seep Carbonates from the Northern South China Sea in Correlation with Fluid Flow

SU Xin1, CHEN Fang2, LU Hong-feng2, HUANG Yong-Yang2   

  1. 1School of Marine Geosciences, China University of Geosciences, Beijing 100083,China;
    2Guangzhou Marine Geological Survey, Guangzhou, Guangdong 510760,China
  • Received:2008-05-10 Revised:2008-06-12 Online:2008-03-20 Published:2008-03-20

Abstract:

A small piece of carbonate concretion collected by research vessel “Haiyang 4” from about 3,000 m seafloor of northern South China Sea was analyzed. The piece of carbonates was identified as methane seep carbonate with 17% magnesium calcites andδ13C value of -61.403‰  and δ18O value of 3.560,6‰. The carbonate shows four micro-textures derived by methane degassing, fluid flow and organisms activities. Calcite rings occur commonly along the walls of vesicles. Inner walls of burrow(worm tubes)are also coated by carbonate rims. Bacterial filaments were found in the fractures or conduits of carbonate, which depended on the methane-rich fluid to survive. Fluid conduits and fractures were often filled by coarser sands, which resulted from fluid flow escaping along these conduits.

Key words: methane seep carbonate, micro-texture, fluid, bacterial filament, South China Sea

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