Kilometre-scale sandstone intrusions in the Eocene of the Outer Moray Firth (UK North Sea): migration paths, reservoirs and potential drilling hazards

Author:

HUUSE M.1,CARTWRIGHT J. A.1,GRAS R.2,HURST A.3

Affiliation:

1. 3DLab, School of Earth, Ocean and Planetary Sciences, Cardiff University, Main Building, Park Place, Cardiff CF10 3YE, Wales, UK (e-mail:m.huuse@earth.cf.ac.uk)

2. Schlumberger Information Solutions, Schlumberger House, Buckingham Gate, Gatwick Airport, West Sussex RH6 0NZ, UK

3. Department of Geology and Petroleum Geology, University of Aberdeen, UK

Abstract

Kilometre-scale sandstone intrusions have recently been documented from the Palaeogene deep-water sequences of the northern North Sea. The distribution of Eocene sandstones within a 126 km23D4C seismic survey located in the Outer Moray Firth was mapped using surface and volume based interpretation of converted wave seismic data calibrated to a number of boreholes. About 35 conical sandstone intrusions, a few tens of metres thick and 1–1.5 km wide, were mapped within the lower Eocene. The intrusions are inclined about 15–20° and crosscut some 100–200 m of lower Eocene mudstones, terminating upward at the Middle Eocene unconformity, below the oil-charged, upper Eocene sandstones of the Alba and Chestnut reservoirs. Individual sandstone intrusions may contain millions of cubic metres of sandstone and often have excellent reservoir properties. Previous studies failed to define a viable migration path for the oil in the Alba/Chestnut reservoirs because they appeared to be completely encased in poorly permeable Eocene mudstones. However, detailed mapping and volume visualization of the converted wave seismic data demonstrates that the upper Eocene reservoirs have suffered post-depositional remobilization and that the conical intrusions provide a viable migration path between the Alba/Chestnut reservoirs and the underlying Paleocene aquifers. Despite more than two decades of exploration activity in the Outer Moray Firth, the widespread occurrence of conical intrusions in the lower Eocene is still not widely recognized, and it is likely that the sandstones may pose a hazard when drilling for deeper targets. However, it is also possible that large conical intrusions that do not connect with overlying sandstones may contain economical quantities of hydrocarbons.Supplementary material:The movie referred to in the article is available athttps://doi.org/10.6084/m9.figshare.c.4812948

Publisher

Geological Society of London

Subject

Fuel Technology,Energy Engineering and Power Technology,Geology,Geochemistry and Petrology

Reference47 articles.

1. Ahmadi Z. M. Sawyers M. Kenyon-Roberts S. Stanworth C. W. Kugler K. A. Kristensen J. Fugelli E. M. G. 2003. Paleocene. In: Evans D. Graham C. Armour A. Bathurst P. (eds) The Millennium Atlas: Petroleum Geology of the Central and Northern North Sea. Geological Society, London, 235–259.

2. Synsedimentary deformation in the Jurassic of southeastern Utah—A case of impact shaking?

3. Historical overview of exploration of Tertiary plays in the UK North Sea

4. Balder and Jotun – two sides of the same coin? A comparison of two Tertiary oil fields in the Norwegian North Sea

5. Polygonal fault systems on the mid-Norwegian margin: a long-term source for fluid flow;Berndt,2003

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