Electrical Identification of Fractures in Oil and Gas Reservoirs: Rock-Physics Foundations, Resistivity Logging, Borehole Imaging, and Intelligent Interpretation
DOI:
https://doi.org/10.54691/sfmnfb63Keywords:
Naturally Fractured Reservoir; Electrical Resistivity; Dual Laterolog; Formation Microimager; Borehole Image Log; Multicomponent Induction; Fracture Aperture; Resistivity Anisotropy; Machine Learning; Formation Evaluation.Abstract
Natural fractures may dominate fluid transport in tight sandstones, carbonates, shales, volcanic rocks, and basement reservoirs despite contributing little bulk porosity. Their electrical signatures are nevertheless non-unique because lithology, fluid salinity, saturation, mud invasion, borehole geometry, and tool sensitivity can reproduce or obscure fracture-related anomalies. This narrative critical review, informed by structured literature searches, links fracture-scale conduction to the responses of conventional resistivity, dual laterolog, multicomponent induction, and electrical borehole imaging tools. The synthesis distinguishes four levels of inference: fracture detection, geometric characterization, potential conductivity, and dynamically confirmed effectiveness. Conductive image traces and deep-shallow resistivity separation can support fracture detection under favorable contrast, whereas position, orientation, and apparent electrical aperture remain tool- and model-dependent estimates. None of these electrical measurements alone establishes reservoir-scale connectivity or permeability. We therefore organize interpretation as a four-stage architecture that conditions the measurements, detects and classifies candidate features, inverts electrical attributes with uncertainty, and tests the resulting hypotheses against core, pressure, mud-loss, sonic, nuclear magnetic resonance, production, or well-test evidence. Automated interpretation may improve consistency, but its field value depends on well-level or field-level external validation and explicit uncertainty calibration. The framework defines which conclusions are directly observed, which are conditional inversions, and which require independent dynamic evidence.
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