Oil charge and biodegradation history in an exhumed fractured reservoir, Devonian, UK

Mas'Ud Baba, John Parnell (Corresponding Author), David Muirhead, Stephen Bowden

Research output: Contribution to journalArticle

3 Citations (Scopus)

Abstract

The distribution of oil residues in fractured Upper Devonian reservoir sandstones of Caithness help us to understand relationships between oil charge and episodes of fracturing. The sandstones are cut by an extensive set of tightly cemented deformation bands in the vicinity of the Brough Fault, and calcite-mineralized open fractures. The deformation bands compartmentalized the reservoir, which subsequently was charged by oil to varying extent in different compartments. Petrographic and biomarker data distinguish two charges of oil. The first charge of oil was unaltered. The later mineralized fractures introduced a heavier biodegraded oil that spread into the sandstone pores and displaced/overprinted the earlier oil. Two distinct oil charges are also evident from two generations of oil fluid inclusions, firstly in overgrowths on quartz grains, and secondly in the calcite veins, exhibiting distinct fluorescence characteristics. Migration and trapping of oil depended on the combination of two fracturing episodes of different character, in which the first episode created sealed compartments which were then filled by oil introduced by the second episode.
Original languageEnglish
Pages (from-to)281-289
Number of pages9
JournalMarine and Petroleum Geology
Volume101
Early online date11 Dec 2018
DOIs
Publication statusPublished - Mar 2019

Fingerprint

biodegradation
oils
histories
oil
history
sandstones
sandstone
fracturing
compartments
calcite
biomarkers
heavy oil
fluid inclusion
veins
trapping
biomarker
fluorescence
quartz
inclusions

Keywords

  • oil charge
  • biodegradation
  • fractured reservoir
  • Devonian
  • Caithness

Cite this

@article{2028ca6fdcfa4eba8bc47bbc9bbf1f8a,
title = "Oil charge and biodegradation history in an exhumed fractured reservoir, Devonian, UK",
abstract = "The distribution of oil residues in fractured Upper Devonian reservoir sandstones of Caithness help us to understand relationships between oil charge and episodes of fracturing. The sandstones are cut by an extensive set of tightly cemented deformation bands in the vicinity of the Brough Fault, and calcite-mineralized open fractures. The deformation bands compartmentalized the reservoir, which subsequently was charged by oil to varying extent in different compartments. Petrographic and biomarker data distinguish two charges of oil. The first charge of oil was unaltered. The later mineralized fractures introduced a heavier biodegraded oil that spread into the sandstone pores and displaced/overprinted the earlier oil. Two distinct oil charges are also evident from two generations of oil fluid inclusions, firstly in overgrowths on quartz grains, and secondly in the calcite veins, exhibiting distinct fluorescence characteristics. Migration and trapping of oil depended on the combination of two fracturing episodes of different character, in which the first episode created sealed compartments which were then filled by oil introduced by the second episode.",
keywords = "oil charge, biodegradation, fractured reservoir, Devonian, Caithness",
author = "Mas'Ud Baba and John Parnell and David Muirhead and Stephen Bowden",
note = "Fluid inclusion data were determined by J. Kelly. JK and MB were in receipt of PhD studentships from the Department of Education (Northern Ireland) and PTDF (Nigeria) respectively. We are grateful to Geology Honours classes from the University of Aberdeen for help in collecting data, and to two constructive reviews of the manuscript.",
year = "2019",
month = "3",
doi = "10.1016/j.marpetgeo.2018.12.024",
language = "English",
volume = "101",
pages = "281--289",
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publisher = "Elsevier",

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T1 - Oil charge and biodegradation history in an exhumed fractured reservoir, Devonian, UK

AU - Baba, Mas'Ud

AU - Parnell, John

AU - Muirhead, David

AU - Bowden, Stephen

N1 - Fluid inclusion data were determined by J. Kelly. JK and MB were in receipt of PhD studentships from the Department of Education (Northern Ireland) and PTDF (Nigeria) respectively. We are grateful to Geology Honours classes from the University of Aberdeen for help in collecting data, and to two constructive reviews of the manuscript.

PY - 2019/3

Y1 - 2019/3

N2 - The distribution of oil residues in fractured Upper Devonian reservoir sandstones of Caithness help us to understand relationships between oil charge and episodes of fracturing. The sandstones are cut by an extensive set of tightly cemented deformation bands in the vicinity of the Brough Fault, and calcite-mineralized open fractures. The deformation bands compartmentalized the reservoir, which subsequently was charged by oil to varying extent in different compartments. Petrographic and biomarker data distinguish two charges of oil. The first charge of oil was unaltered. The later mineralized fractures introduced a heavier biodegraded oil that spread into the sandstone pores and displaced/overprinted the earlier oil. Two distinct oil charges are also evident from two generations of oil fluid inclusions, firstly in overgrowths on quartz grains, and secondly in the calcite veins, exhibiting distinct fluorescence characteristics. Migration and trapping of oil depended on the combination of two fracturing episodes of different character, in which the first episode created sealed compartments which were then filled by oil introduced by the second episode.

AB - The distribution of oil residues in fractured Upper Devonian reservoir sandstones of Caithness help us to understand relationships between oil charge and episodes of fracturing. The sandstones are cut by an extensive set of tightly cemented deformation bands in the vicinity of the Brough Fault, and calcite-mineralized open fractures. The deformation bands compartmentalized the reservoir, which subsequently was charged by oil to varying extent in different compartments. Petrographic and biomarker data distinguish two charges of oil. The first charge of oil was unaltered. The later mineralized fractures introduced a heavier biodegraded oil that spread into the sandstone pores and displaced/overprinted the earlier oil. Two distinct oil charges are also evident from two generations of oil fluid inclusions, firstly in overgrowths on quartz grains, and secondly in the calcite veins, exhibiting distinct fluorescence characteristics. Migration and trapping of oil depended on the combination of two fracturing episodes of different character, in which the first episode created sealed compartments which were then filled by oil introduced by the second episode.

KW - oil charge

KW - biodegradation

KW - fractured reservoir

KW - Devonian

KW - Caithness

UR - http://www.mendeley.com/research/oil-charge-biodegradation-history-exhumed-fractured-reservoir-devonian-uk

U2 - 10.1016/j.marpetgeo.2018.12.024

DO - 10.1016/j.marpetgeo.2018.12.024

M3 - Article

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EP - 289

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SN - 0264-8172

ER -