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by Abdulkarim MA, Muxworthy AR and Fraser A (2022) Front. Earth Sci. 10:973385. doi: 10.3389/feart.2022.973385
Due to a production error, an incorrect version of Figure 5 was included in the published article. The correct version of Figure 5 appears below. The publisher apologizes for this mistake.
FIGURE 5
FIGURE 5. Example results from the HT-χ measurements carried out on the Bonneville samples. The magnetic minerology of the “main” oil leg is dominated by siderite. The oil-water region presents a diminished siderite signature and the presence of hexagonal pyrrhotite. Note that the oil-water contact (OWC) marked is as obtained via well logs and pressure analysis.
The original version of this article has been updated.
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Keywords: magnetic mineral diagenesis, oil water contact, oil-water transition zone, magnetic method, UK Central North Sea, biodegradation, hydrolysis
Citation: Frontiers Production Office (2023) Erratum: High temperature susceptibility measurements: A potential tool for the identification of oil water transition zone in petroleum reservoirs. Front. Earth Sci. 10:1118266. doi: 10.3389/feart.2022.1118266
Received: 07 December 2022; Accepted: 07 December 2022;
Published: 04 January 2023.
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