Explores the origin of Gilmore gas, revealing deep-sourced methane and its implications for gas reservoir geology.
The origin of the Gilmore dry gas deposit is a combination of deep-sourced methane and wet gas associated with oil generation. The deep gas source is characterised by the high nitrogen content co-generated with isotopically heavy methane. Higher nitrogen contents (up to 20 mole%) occur along the eastern margin of the Lissoy Sandstone principal reservoir unit, supporting reservoir compartmentalisation.
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Australia) et al. (1997) studied this question.
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