2010
DOI: 10.1016/j.marpetgeo.2009.08.005
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Surface sediment gases as indicators of subsurface hydrocarbons – examining the record in laboratory and field studies

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Cited by 20 publications
(37 citation statements)
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“…Gases derived from these different processes will display a distinctive hydrocarbon and non-hydrocarbon composition and compound-specific isotopic signature. Examination of seabed geochemical signatures from worldwide surveys suggest the near-surface sediment gas and isotopic signatures are different than expected due to in situ microbial alteration, partitioning between vapour, solute, and sorbed phases, mixing with gases from multiple origins, degassing fractionation from sample collection and fractionation related to the gas extraction method [2,3].…”
Section: Introductionmentioning
confidence: 98%
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“…Gases derived from these different processes will display a distinctive hydrocarbon and non-hydrocarbon composition and compound-specific isotopic signature. Examination of seabed geochemical signatures from worldwide surveys suggest the near-surface sediment gas and isotopic signatures are different than expected due to in situ microbial alteration, partitioning between vapour, solute, and sorbed phases, mixing with gases from multiple origins, degassing fractionation from sample collection and fractionation related to the gas extraction method [2,3].…”
Section: Introductionmentioning
confidence: 98%
“…Sediment gases can reside in the interstitial spaces, bound to mineral or organic surfaces, and/or entrapped in carbonate inclusions [2,3]. The interstitial sediment gases are those gases contained within the sediment pore space, either dissolved in the pore waters (solute) or as free gas (vapour) [4].…”
Section: Introductionmentioning
confidence: 99%
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