Petroleum generation and migration through the Faroe–Shetland Basin – the role of igneous intrusions

Author:

Mangione A.1ORCID,Schofield N.1,Holford S.2,Grove C.3,Ellis C.3,Forster C.3,Schenk O.4,Gardiner D.5,Hedley B.6,Broadley L.7,Underhill J. R.1

Affiliation:

1. Department of Geology and Petroleum Geology, University of Aberdeen, King's College, Aberdeen AB24 3FX, UK

2. School of Physics, Chemistry and Earth Sciences, University of Adelaide, North Terrace Campus, Adelaide, SA 5005, Australia

3. Siccar Point Energy Ltd (now Ithaca Energy (UK) Ltd), Hill of Rubislaw, Aberdeen AB15 6BY, UK

4. Schlumberger, Ritterstraße 23, 52072 Aachen, Germany

5. Integrated Geochemical Interpretation Ltd, The Granary, Hallsannery, Devon EX39 5HE, UK

6. Dana Petroleum Ltd, 62 Huntly Street, Aberdeen AB10 1RS, UK

7. Spirit Energy Ltd, 15 Justice Mill Lane, Aberdeen AB11 6EQ, UK

Abstract

Previous basin modelling of the Faroe–Shetland Basin (FSB, offshore UK) has suggested mid-Cretaceous petroleum generation, which predates the deposition of the working Paleogene reservoirs and traps. To justify the time discrepancy between generation, reservoir, and trap formation, factors such as intermediary accumulations and overpressure have been invoked. However, across much of the FSB, the Cretaceous sequences that overly the Kimmeridgian source rock are heavily intruded by Paleogene-aged intrusions. Recent modelling has shown that the emplacement of the intrusions, coupled with lower radiogenic heat production from underlying basement, leads to estimates of petroleum generation occurring up to 40 myr more recently than suggested by previous models. In this work, we seek to better understand the role that igneous intrusions have exerted on petroleum generation and migration in the FSB. Models with varying thicknesses of Paleogene intrusions are compared with those that consider the Cretaceous sequence as purely sedimentary (i.e. similar to assumptions in previous modelling). The estimated times of petroleum generation are compared with geochronological constraints on the ages of oils (i.e. c . 90–68 Ma) along with the deposition and formation of other petroleum system elements. By considering only the effect of igneous intrusions, the expulsion onset from the source rock is retarded by up to 12 myr. In addition, our models show the impact of the intrusions on petroleum saturation and migration, suggesting that intrusions have potentially compartmentalized the basin, trapping petroleum beneath or within the sill complex. Finally, our findings suggest that basin models in regions impacted by significant magmatism need to consider the impact of intrusions to more accurately constrain both petroleum generation and migration. Thematic collection: This article is part of the New learning from exploration and development in the UKCS Atlantic Margin collection available at: https://www.lyellcollection.org/topic/collections/new-learning-from-exploration-and-development-in-the-ukcs-atlantic-margin

Publisher

Geological Society of London

Subject

Earth and Planetary Sciences (miscellaneous),Economic Geology,Geochemistry and Petrology,Geology,Fuel Technology

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5. Some practical guidance for petroleum migration modeling

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