Predicting fluid pressure in sedimentary basins from seismic tomography

10 pages, 9 figures, 2 tables.-- Geophysical Journal International ©: 2019 Predicting fluid pressure in sedimentary basins from seismic tomography Published by Oxford University Press on behalf of the Royal Astronomical Society. All rights reserved Gravitational compaction of thick (2-10 km) sedimen...

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Published in:Geophysical Journal International
Main Authors: O'Reilly, Brian M., Prada, Manel, Lavoué, François, Lebedev, Sergei
Other Authors: Science Foundation Ireland, European Commission
Format: Article in Journal/Newspaper
Language:unknown
Published: Oxford University Press 2019
Subjects:
Online Access:http://hdl.handle.net/10261/195134
https://doi.org/10.1093/gji/ggz378
https://doi.org/10.13039/501100001602
https://doi.org/10.13039/501100000780
id ftcsic:oai:digital.csic.es:10261/195134
record_format openpolar
spelling ftcsic:oai:digital.csic.es:10261/195134 2024-02-11T10:06:46+01:00 Predicting fluid pressure in sedimentary basins from seismic tomography O'Reilly, Brian M. Prada, Manel Lavoué, François Lebedev, Sergei Science Foundation Ireland European Commission 2019-11 http://hdl.handle.net/10261/195134 https://doi.org/10.1093/gji/ggz378 https://doi.org/10.13039/501100001602 https://doi.org/10.13039/501100000780 unknown Oxford University Press Publisher's version https://doi.org/10.1093/gji/ggz378 No issn: 0956-540X e-issn: 1365-246X Geophysical Journal International 219(2): 1421-143 (2019) http://hdl.handle.net/10261/195134 doi:10.1093/gji/ggz378 http://dx.doi.org/10.13039/501100001602 http://dx.doi.org/10.13039/501100000780 open Seismic tomography Europe Sedimentary basin processes Permeability and porosity artículo http://purl.org/coar/resource_type/c_6501 2019 ftcsic https://doi.org/10.1093/gji/ggz37810.13039/50110000160210.13039/501100000780 2024-01-16T10:45:46Z 10 pages, 9 figures, 2 tables.-- Geophysical Journal International ©: 2019 Predicting fluid pressure in sedimentary basins from seismic tomography Published by Oxford University Press on behalf of the Royal Astronomical Society. All rights reserved Gravitational compaction of thick (2-10 km) sediment accumulations in sedimentary basins is controlled by the interplay of mechanical and chemical processes that operate over many orders of magnitude in spatial scale. The compaction of sediments into rock typically involves a density increase of ≈500 to 1000 kg m−3, occurring over a depth-scale of several kilometres. The volume decrease in the compacting sediments releases vast volumes of water, which plays an important part in the global hydrological cycle and also in tectonic and geochemical processes; including the formation of hydrocarbon and mineral deposits. This study utilizes recently developed tomographic seismic images from the Porcupine Basin, which lies in the deep-water North Atlantic Ocean. A generic method for predicting fluid pressure variations that are driven by gravitational compaction is developed over the scale of the entire sedimentary basin. The methodology is grounded upon both observational evidence and empirically based theories, relying on geophysical measurements and relationships between sediment porosities and densities. The method is based upon physical concepts that are widely used in the petroleum industry and applied extensively in models of overpressure development in sedimentary basins. Geological and geophysical data from exploration wells are used to test the predictions of the method at two locations within the basin and are found to be in good agreement with the theory This publication has emanated from research supported in part by a research grant from Science Foundation Ireland (SFI) under Grant Number 13/RC/2092 and is cofunded under the European Regional Development Fund and by PIPCO RSG and its member companies Peer Reviewed Article in Journal/Newspaper North Atlantic Digital.CSIC (Spanish National Research Council) Geophysical Journal International 219 2 1421 1430
institution Open Polar
collection Digital.CSIC (Spanish National Research Council)
op_collection_id ftcsic
language unknown
topic Seismic tomography
Europe
Sedimentary basin processes
Permeability and porosity
spellingShingle Seismic tomography
Europe
Sedimentary basin processes
Permeability and porosity
O'Reilly, Brian M.
Prada, Manel
Lavoué, François
Lebedev, Sergei
Predicting fluid pressure in sedimentary basins from seismic tomography
topic_facet Seismic tomography
Europe
Sedimentary basin processes
Permeability and porosity
description 10 pages, 9 figures, 2 tables.-- Geophysical Journal International ©: 2019 Predicting fluid pressure in sedimentary basins from seismic tomography Published by Oxford University Press on behalf of the Royal Astronomical Society. All rights reserved Gravitational compaction of thick (2-10 km) sediment accumulations in sedimentary basins is controlled by the interplay of mechanical and chemical processes that operate over many orders of magnitude in spatial scale. The compaction of sediments into rock typically involves a density increase of ≈500 to 1000 kg m−3, occurring over a depth-scale of several kilometres. The volume decrease in the compacting sediments releases vast volumes of water, which plays an important part in the global hydrological cycle and also in tectonic and geochemical processes; including the formation of hydrocarbon and mineral deposits. This study utilizes recently developed tomographic seismic images from the Porcupine Basin, which lies in the deep-water North Atlantic Ocean. A generic method for predicting fluid pressure variations that are driven by gravitational compaction is developed over the scale of the entire sedimentary basin. The methodology is grounded upon both observational evidence and empirically based theories, relying on geophysical measurements and relationships between sediment porosities and densities. The method is based upon physical concepts that are widely used in the petroleum industry and applied extensively in models of overpressure development in sedimentary basins. Geological and geophysical data from exploration wells are used to test the predictions of the method at two locations within the basin and are found to be in good agreement with the theory This publication has emanated from research supported in part by a research grant from Science Foundation Ireland (SFI) under Grant Number 13/RC/2092 and is cofunded under the European Regional Development Fund and by PIPCO RSG and its member companies Peer Reviewed
author2 Science Foundation Ireland
European Commission
format Article in Journal/Newspaper
author O'Reilly, Brian M.
Prada, Manel
Lavoué, François
Lebedev, Sergei
author_facet O'Reilly, Brian M.
Prada, Manel
Lavoué, François
Lebedev, Sergei
author_sort O'Reilly, Brian M.
title Predicting fluid pressure in sedimentary basins from seismic tomography
title_short Predicting fluid pressure in sedimentary basins from seismic tomography
title_full Predicting fluid pressure in sedimentary basins from seismic tomography
title_fullStr Predicting fluid pressure in sedimentary basins from seismic tomography
title_full_unstemmed Predicting fluid pressure in sedimentary basins from seismic tomography
title_sort predicting fluid pressure in sedimentary basins from seismic tomography
publisher Oxford University Press
publishDate 2019
url http://hdl.handle.net/10261/195134
https://doi.org/10.1093/gji/ggz378
https://doi.org/10.13039/501100001602
https://doi.org/10.13039/501100000780
genre North Atlantic
genre_facet North Atlantic
op_relation Publisher's version
https://doi.org/10.1093/gji/ggz378
No
issn: 0956-540X
e-issn: 1365-246X
Geophysical Journal International 219(2): 1421-143 (2019)
http://hdl.handle.net/10261/195134
doi:10.1093/gji/ggz378
http://dx.doi.org/10.13039/501100001602
http://dx.doi.org/10.13039/501100000780
op_rights open
op_doi https://doi.org/10.1093/gji/ggz37810.13039/50110000160210.13039/501100000780
container_title Geophysical Journal International
container_volume 219
container_issue 2
container_start_page 1421
op_container_end_page 1430
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