Seismic and structural characterization of fluid escape pipes using 3D and partial stack seismic from the Loyal field (UK): A multiphase and repeated intrusive mechanism

Daniele Maestrelli, David Iacopini, Ali Jihad, Clare E. Bond, Marco Bonini

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Abstract

The potential for fluid leakage from sub-surface reservoirs has important implications for CO2 storage, hydrocarbon reservoirs and water resources. Understanding the genesis, morphology, fluid flow mechanisms and extent of fluid escape from reservoirs allows for better risking of geological resources and storage potential. Here we describe in detail the structures of fluid escape pipes from the Loyal field, observed from a 3D full and partial stack seismic dataset. The seismic imagery suggests that the fluid escape pipes are rooted at least in the main Paleocene reservoir and by-pass the reservoir seal to cross the post Lista Formation overburden up to the intra-Neogene units. The pipes extend for a few hundred meters to a few kilometres and show a varying shape structures from blow-out structures to incipient mud volcanoes. The structural relation of the pipes termination suggest they were active between the formation of Neogene faults and fractures and the erosive event related to the Intra-Neogene unconformity. A detailed analysis of the seismic characteristics observed both from main baseline and partial stack data allows a division of the pipes into two families: (1) seeps and pipes following structural discontinuities (2) pipes unrelated to the pre-existing structural features. The pipes internal seismic response, the reflector termination of the main conduits and the distribution of stacked bright reflectors suggests an upward migration mechanism (during pipe birth and development), requiring a cyclic switching from non-Darcy hydrofracturing (during overpressure) to Darcy flow lateral migration (during low-pressure stage). The improved understanding of the seal by pass structure affecting the overburden structure will allow for better de-risking of the geological area and improve the velocity model of the overburden in the study area.
Original languageEnglish
Pages (from-to)489-510
Number of pages22
JournalMarine and Petroleum Geology
Volume88
Early online date14 Aug 2017
DOIs
Publication statusPublished - Dec 2017

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escape
pipe
fluid
fluids
overburden
Neogene
reflectors
resources
stack
water resources
mud volcano
overpressure
mud
hydrocarbon reservoir
seismic response
imagery
volcanoes
Paleocene
unconformity
division

Keywords

  • Fluid escape pipe
  • Mud intrusion
  • Fluid leakage
  • 3D seismic
  • Loyal Field
  • North Sea

Cite this

Seismic and structural characterization of fluid escape pipes using 3D and partial stack seismic from the Loyal field (UK) : A multiphase and repeated intrusive mechanism. / Maestrelli, Daniele; Iacopini, David; Jihad, Ali; Bond, Clare E.; Bonini, Marco.

In: Marine and Petroleum Geology, Vol. 88, 12.2017, p. 489-510.

Research output: Contribution to journalArticle

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title = "Seismic and structural characterization of fluid escape pipes using 3D and partial stack seismic from the Loyal field (UK): A multiphase and repeated intrusive mechanism",
abstract = "The potential for fluid leakage from sub-surface reservoirs has important implications for CO2 storage, hydrocarbon reservoirs and water resources. Understanding the genesis, morphology, fluid flow mechanisms and extent of fluid escape from reservoirs allows for better risking of geological resources and storage potential. Here we describe in detail the structures of fluid escape pipes from the Loyal field, observed from a 3D full and partial stack seismic dataset. The seismic imagery suggests that the fluid escape pipes are rooted at least in the main Paleocene reservoir and by-pass the reservoir seal to cross the post Lista Formation overburden up to the intra-Neogene units. The pipes extend for a few hundred meters to a few kilometres and show a varying shape structures from blow-out structures to incipient mud volcanoes. The structural relation of the pipes termination suggest they were active between the formation of Neogene faults and fractures and the erosive event related to the Intra-Neogene unconformity. A detailed analysis of the seismic characteristics observed both from main baseline and partial stack data allows a division of the pipes into two families: (1) seeps and pipes following structural discontinuities (2) pipes unrelated to the pre-existing structural features. The pipes internal seismic response, the reflector termination of the main conduits and the distribution of stacked bright reflectors suggests an upward migration mechanism (during pipe birth and development), requiring a cyclic switching from non-Darcy hydrofracturing (during overpressure) to Darcy flow lateral migration (during low-pressure stage). The improved understanding of the seal by pass structure affecting the overburden structure will allow for better de-risking of the geological area and improve the velocity model of the overburden in the study area.",
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note = "Acknowledgements We thank an anonymous reviewer for the several constructive comments. The seismic interpretation and image processing was carried out in the SeisLab facility at the University of Aberdeen (sponsored by BG BP and Chevron). Seismic imaging analysis was performed using GeoTeric{\circledR} (ffA), and analysis of seismic amplitudes was performed in Petrel{\circledR} 2016 (Schlumberger). We would like to thank the Tuscany PhD Regional program and the Erasmus+exchange for funding the Aberdeen permanence of one of us (D.M.). Gazprom for supporting A.J PhD., BP for the release of the Loyal field seismic dataset utilized in this research paper and also N.Vanden Beukel (BP) and M. Gorling (BP) and his colleagues for their assistance.",
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AU - Bond, Clare E.

AU - Bonini, Marco

N1 - Acknowledgements We thank an anonymous reviewer for the several constructive comments. The seismic interpretation and image processing was carried out in the SeisLab facility at the University of Aberdeen (sponsored by BG BP and Chevron). Seismic imaging analysis was performed using GeoTeric® (ffA), and analysis of seismic amplitudes was performed in Petrel® 2016 (Schlumberger). We would like to thank the Tuscany PhD Regional program and the Erasmus+exchange for funding the Aberdeen permanence of one of us (D.M.). Gazprom for supporting A.J PhD., BP for the release of the Loyal field seismic dataset utilized in this research paper and also N.Vanden Beukel (BP) and M. Gorling (BP) and his colleagues for their assistance.

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N2 - The potential for fluid leakage from sub-surface reservoirs has important implications for CO2 storage, hydrocarbon reservoirs and water resources. Understanding the genesis, morphology, fluid flow mechanisms and extent of fluid escape from reservoirs allows for better risking of geological resources and storage potential. Here we describe in detail the structures of fluid escape pipes from the Loyal field, observed from a 3D full and partial stack seismic dataset. The seismic imagery suggests that the fluid escape pipes are rooted at least in the main Paleocene reservoir and by-pass the reservoir seal to cross the post Lista Formation overburden up to the intra-Neogene units. The pipes extend for a few hundred meters to a few kilometres and show a varying shape structures from blow-out structures to incipient mud volcanoes. The structural relation of the pipes termination suggest they were active between the formation of Neogene faults and fractures and the erosive event related to the Intra-Neogene unconformity. A detailed analysis of the seismic characteristics observed both from main baseline and partial stack data allows a division of the pipes into two families: (1) seeps and pipes following structural discontinuities (2) pipes unrelated to the pre-existing structural features. The pipes internal seismic response, the reflector termination of the main conduits and the distribution of stacked bright reflectors suggests an upward migration mechanism (during pipe birth and development), requiring a cyclic switching from non-Darcy hydrofracturing (during overpressure) to Darcy flow lateral migration (during low-pressure stage). The improved understanding of the seal by pass structure affecting the overburden structure will allow for better de-risking of the geological area and improve the velocity model of the overburden in the study area.

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JO - Marine and Petroleum Geology

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