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SEISMIC IMAGING OF SUBSURFACE FLUID FLOW: PETROLEUM SYSTEMS AND SHALLOW HAZARDS Dr Mads Huuse Project Summary Fluid flow in sedimentary basins occurs within aquifers, by diffuse flow through pore networks in mudstones and through focused conduits, bypassing both aquifers and pore networks. The ubiquitous presence and significance of such focused conduits, termed ‘seal bypass systems’, has only recently been discovered by means of high-resolution 3D seismic analysis (Cartwright et al. 2007). Seal-bypass systems analysis provides evidence of hydrocarbon systems and helps in the identification of shallow hazards including shallow gas, mud volcano systems, flow sands and gas hydrate accumulations. This project aims to further the research into the origin and significance of seal-bypass systems by integrating analysis of hi-quality 3D seismic images offshore West Africa with seafloor and sea-surface evidence for fluid expulsion, thus examining both the plumbing system within the shallow crust and the fluids that are passing through the plumbing system from deeply buried source rocks and reservoirs to the seafloor. The integration of 3D seismic data, seafloor samples and satellite seep detection will allow a spatio-temporal reconstruction of past and present fluid flow at an unprecedented areal extent and level of detail and should allow an assessment of the dynamic nature of shallow subsurface fluid migration and storage under glacial and interglacial conditions (low and high eustatic levels). The analysis will involve extensive 3D seismic interpretation, seismic geomorphological analysis, integration with seep geochemistry and satellite imagery using both subsurface interpretation and geo- spatial analysis software and is thus well suited to a candidate with a broad geosciences background. For further details contact: [email protected] References: Andresen, K.J., Huuse, M., Schødt, N.H., Clausen, L.F. & Seidler, L. 2011. Hydrocarbon plumbing systems of salt minibasins offshore Angola revealed by three-dimensional seismic analysis. AAPG Bulletin, 95(6), 1039-1065. Calves, G., Huuse, M., Schwab, A.M. & Clift, P.D. 2008. 3D seismic analysis of high-amplitude anomalies in the shallow subsurface of the Northern Indus Fan: sedimentary and/or fluid origin. Journal of Geophysical Research, 113, B11103, doi:10.1029/2008JB005666. Cartwright, J., Huuse, M. & Aplin, A. 2007. Seal bypass systems. AAPG Bulletin, 91, 1141-1166. Huuse, M., Jackson, C.A., Van Rensbergen, P., Davies, R.J., Flemings, P.B. & Dixon, R.J. 2010. Subsurface sediment remobilization and fluid flow in sedimentary basins: An overview. Basin Research, 22(4), 342-360. Serie, C., Huuse, M. & Schødt, N.H. in press. Gas hydrate pingoes: Deep seafloor evidence of focused fluid flow on continental margins. Geology, in press.

Seismic Imaging of Subsurface Fluid Flow Petroleum Systems and Shallow Hazards

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  • SEISMIC IMAGING OF SUBSURFACE FLUID FLOW: PETROLEUM SYSTEMS AND SHALLOW HAZARDS

    Dr Mads Huuse

    Project Summary Fluid flow in sedimentary basins occurs within aquifers, by diffuse flow through pore networks in mudstones and through focused conduits, bypassing both aquifers and pore networks. The ubiquitous presence and significance of such focused conduits, termed seal bypass systems, has only recently been discovered by means of high-resolution 3D seismic analysis (Cartwright et al. 2007). Seal-bypass systems analysis provides evidence of hydrocarbon systems and helps in the identification of shallow hazards including shallow gas, mud volcano systems, flow sands and gas hydrate accumulations. This project aims to further the research into the origin and significance of seal-bypass systems by integrating analysis of hi-quality 3D seismic images offshore West Africa with seafloor and sea-surface evidence for fluid expulsion, thus examining both the plumbing system within the shallow crust and the fluids that are passing through the plumbing system from deeply buried source rocks and reservoirs to the seafloor. The integration of 3D seismic data, seafloor samples and satellite seep detection will allow a spatio-temporal reconstruction of past and present fluid flow at an unprecedented areal extent and level of detail and should allow an assessment of the dynamic nature of shallow subsurface fluid migration and storage under glacial and interglacial conditions (low and high eustatic levels). The analysis will involve extensive 3D seismic interpretation, seismic geomorphological analysis, integration with seep geochemistry and satellite imagery using both subsurface interpretation and geo-spatial analysis software and is thus well suited to a candidate with a broad geosciences background. For further details contact: [email protected] References: Andresen, K.J., Huuse, M., Schdt, N.H., Clausen, L.F. & Seidler, L. 2011. Hydrocarbon plumbing systems of salt minibasins offshore Angola revealed by three-dimensional seismic analysis. AAPG Bulletin, 95(6), 1039-1065. Calves, G., Huuse, M., Schwab, A.M. & Clift, P.D. 2008. 3D seismic analysis of high-amplitude anomalies in the shallow subsurface of the Northern Indus Fan: sedimentary and/or fluid origin. Journal of Geophysical Research, 113, B11103, doi:10.1029/2008JB005666. Cartwright, J., Huuse, M. & Aplin, A. 2007. Seal bypass systems. AAPG Bulletin, 91, 1141-1166. Huuse, M., Jackson, C.A., Van Rensbergen, P., Davies, R.J., Flemings, P.B. & Dixon, R.J. 2010. Subsurface sediment remobilization and fluid flow in sedimentary basins: An overview. Basin Research, 22(4), 342-360. Serie, C., Huuse, M. & Schdt, N.H. in press. Gas hydrate pingoes: Deep seafloor evidence of focused fluid flow on continental margins. Geology, in press.