Petroleum generation and migration in the Cambro-Ordovician Laurentian margin succession of NW Scotland

Parnell, J., Bowden, S. and Mark, D. (2018) Petroleum generation and migration in the Cambro-Ordovician Laurentian margin succession of NW Scotland. Journal of the Geological Society, 175(1), pp. 33-42. (doi: 10.1144/jgs2017-059)

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Abstract

Fluid inclusion and organic biomarker data show that there was formerly a hydrocarbon system in the CambroOrdovician Laurentian margin rocks of NW Scotland. Oil fluid inclusions occur in stylolitized Eriboll Formation sandstone, in K-feldspar cements with an 40Ar/39Ar age of 415 ± 5.5/5.8 Ma (2σ, analytical precision/full external precision). Organic extracts from Durness Group black limestones yield biomarker ratios characteristic of high thermal maturity. Organic maturation to yield oil probably occurred during orogenic deformation along the Moine Thrust Zone. The recognition of a hydrocarbon system in Scotland adds to a huge hydrocarbon province in Laurentian rocks including North America and Greenland.

Item Type:Articles
Status:Published
Refereed:Yes
Glasgow Author(s) Enlighten ID:Mark, Professor Darren
Authors: Parnell, J., Bowden, S., and Mark, D.
College/School:College of Science and Engineering > Scottish Universities Environmental Research Centre
Journal Name:Journal of the Geological Society
Publisher:Geological Society of London
ISSN:0016-7649
ISSN (Online):2041-479X
Published Online:02 October 2017
Copyright Holders:Copyright © 2017 The Authors
First Published:First published in Journal of the Geological Society 175(1):33-43
Publisher Policy:Reproduced under a Creative Commons License
Data DOI:10.6084/m9.figshare.c.3879616

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