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istry to reveal the hydrocarbon potential, the extent of diagenesis and organic matter type of the formation analysed. Sea floor cores are also analysed using this technique for the purpose of gas seep survey and gas hydrate study. In this study, drilling cuttings from a well, western offshore Taiwan was collected and analysed. The hydrocarbon content and composition in the encountered formation indicates that the Miocene coal-bearing formations are of excellent organic richness. The onset of the thermogenic hydrocarbons is at 2000 m in depth based on the wet gases ratio. Major organic matter in the encountered formations is gas-prone, judged from their low C5 + content. Hydrocarbon gas in the sea floor sediments collected from southwestern offshore Taiwan is in several hundreds ppm, with methane dominated. C2 + are present but in low concentration, implying that the gas in the sediments is mainly of biogenic and mixed with some thermo-genic gas vertical migrated from deeper and more mature formation. The gas in the gas hydrates supposed occurred in this area is believed to have similar composition and origin to the gas analysed. ## Hydrogen generation from water electrolysispossib

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Publisher

Elsevier Science; Elsevier ; Elsevier BV (ISSN 0140-6701)

Published

2004

Language

EN

Field

Engineering (Physical Sciences)