Evaluation of total organic carbon distinguishes source rock quality in Lorraine Coal Basin using geophysical well-logs, indicating exploration potential.
The Lorraine Coal Basin, recognized as the most promising coal bed methane basin in France and Europe, holds significance for the energy transition after more than a century of coal mining until 2004 and renewed interest in oil and gas exploration in the 80s and 90s. New data from an on-going exploration campaign within this basin facilitates the assessment of gas resources embedded in sedimentary deposits. This evaluation is achieved by determining Total Organic Carbon (TOC) along wells, using well-log data. The study employs a methodology encompassing Schmoker’s method, Δ log R, and multivariate regression, focusing on two reference boreholes, namely Fols 1A and Dbl S1. Schmoker’s method provides the most accurate TOC values, consistent with Rock-Eval data. However, the Δ log R method underestimates TOC values, particularly for coal lithologies, for which logarithmic equations are proposed for proportional corrections. Moreover, new equations based on multivariate regression of gamma-ray, sonic, and resistivity logs are developed for TOC estimation. Schmoker’s method proves to be the most reliable with available density logs in the Lorraine Coal Basin. Alternatively, the modified Δ log R equations or those derived from the multivariate regression of gamma-ray, sonic, and resistivity logs can be used. Based on TOC, lithologies of the investigated sedimentary series may be classified from lean to fair source-rocks for shaly lithologies to excellent for the coal layer.
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Allouti et al. (2025) studied this question.
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