4.6 Article

Using magnetic techniques to calibrate hydrocarbon migration in petroleum systems modelling: a case study from the Lower Tertiary, UK Central North Sea

Journal

GEOPHYSICAL JOURNAL INTERNATIONAL
Volume 227, Issue 1, Pages 617-631

Publisher

OXFORD UNIV PRESS
DOI: 10.1093/gji/ggab236

Keywords

Europe; Environmental magnetism; Magnetic mineralogy and petrology; Rock and mineral magnetism

Funding

  1. Petroleum Technology Development Fund (PTDF) Nigeria
  2. National Science Foundation
  3. University of Minnesota

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This study investigates the potential of magnetic minerals as a proxy for hydrocarbon migration pathways by testing core samples from the Tay Fan in the Central North Sea. Results show a variety of magnetic minerals present in similar concentrations, with an increasing presence of authigenic iron sulphides along the identified lateral hydrocarbon migration pathway. This suggests mineral magnetic techniques could be used to quickly identify biodegradation severity or oil maturity in core samples, which can then be used to calibrate petroleum systems models.
Magnetic minerals form or alter in the presence of hydrocarbons, making them a potential magnetic proxy for identifying hydrocarbon migration pathways. In this paper, we test this idea by magnetically measuring core samples from the Tay Fan in theWestern Central Graben in the Central North Sea. In a companion paper, 3-D petroleum systems modelling has been carried out to forward model migration pathways within the Tay Fan. Rock magnetic experiments identified a range of magnetite, maghemite, iron sulphides, siderite, goethite and titanohematite, some of which are part of the background signal, and some due to the presence of hydrocarbons. Typical concentrations of the magnetic minerals were similar to 10-200 ppm. Importantly, we have identified an increasing presence of authigenic iron sulphides (likely pyrite and greigite) along the identified lateral hydrocarbon migration pathway (east to west). This is likely caused by biodegradation resulting in the precipitation of iron sulphides, however, though less likely, it could alternatively be caused by mature oil generation, which subsequently travelled with the migrating oil to the traps in the west. These observations suggest mineral magnetic techniques could be a rapid alternative method for identifying the severity of biodegradation or oil maturity in core sample, which can then be used to calibrate petroleum systems models.

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