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The nature and age of basement host rocks and fissure fills in the Lancaster field fractured reservoir, West of Shetland

Holdsworth, R. E.; Trice, R.; Hardman, K.; McCaffrey, K. J.W.; Morton, A.; Frei, D.; Dempsey, E.; Bird, A.; Rogers, S.

Authors

R. E. Holdsworth

R. Trice

K. Hardman

K. J.W. McCaffrey

A. Morton

D. Frei

Profile image of Eddie Dempsey

Dr Eddie Dempsey E.Dempsey@hull.ac.uk
Senior Lecturer in Structural Geology and Geohazards

S. Rogers



Abstract

Hosting up to 3.3 billion barrels of oil in place, the upfaulted Precambrian crystalline rocks of the Lancaster field, offshore west of Shetland, give key insights into how fractured hydrocarbon reservoirs can form in such old rocks. The Neoarchean (c. 2700–2740 Ma) charnockitic basement is cut by deeply penetrating oil-, mineral-and sediment-filled fissure systems seen in geophysical and production logs and thin sections of core. Mineral textures and fluid inclusion geothermometry suggest that a low-temperature (<200°C) near-surface hydrothermal system is associated with these fissures. The fills help to permanently prop open fissures in the basement, permitting the ingress of hydrocarbons into extensive well-connected oil-saturated fracture networks. U–Pb dating of calcite mineral fills constrains the onset of mineralization and contemporaneous oil charge to the mid-Cretaceous and later from Jurassic source rocks flanking the upfaulted ridge. Late Cretaceous subsidence and deposition of mudstones sealed the ridge, and was followed by buoyancy-driven migration of oil into the pre-existing propped fracture systems. These new observations provide an explanation for the preservation of intra-reservoir fractures (‘joints’) with effective apertures of 2 m or more, thereby highlighting a new mechanism for generating and preserving fracture permeability in sub-unconformity fractured basement reservoirs worldwide.

Citation

Holdsworth, R. E., Trice, R., Hardman, K., McCaffrey, K. J., Morton, A., Frei, D., Dempsey, E., Bird, A., & Rogers, S. (2020). The nature and age of basement host rocks and fissure fills in the Lancaster field fractured reservoir, West of Shetland. Journal of the Geological Society, 177(5), 1057-1073. https://doi.org/10.1144/jgs2019-142

Journal Article Type Article
Acceptance Date Nov 22, 2019
Online Publication Date Nov 29, 2019
Publication Date Nov 1, 2020
Deposit Date Nov 25, 2019
Publicly Available Date Dec 3, 2019
Journal Journal of the Geological Society
Print ISSN 0016-7649
Publisher The Geological Society
Peer Reviewed Peer Reviewed
Volume 177
Issue 5
Pages 1057-1073
DOI https://doi.org/10.1144/jgs2019-142
Keywords Geology
Public URL https://hull-repository.worktribe.com/output/3242227
Contract Date Dec 3, 2019

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