Lithological constraints on borehole wall failure: a study on the Pennine Coal Measures of the United Kingdom
Fellgett, Mark W.; Kingdon, Andrew ORCID: https://orcid.org/0000-0003-4979-588X; Waters, Colin N.; Field, Lorraine; Shreeve, James; Dobbs, Marcus; Ougier-Simonin, Audrey. 2019 Lithological constraints on borehole wall failure: a study on the Pennine Coal Measures of the United Kingdom. Frontiers in Earth Science, 7, 163. 10.3389/feart.2019.00163
Before downloading, please read NORA policies.Preview |
Text (Open Access Paper)
feart-07-00163.pdf - Published Version Available under License Creative Commons Attribution 4.0. Download (14MB) | Preview |
Abstract/Summary
Stress-related borehole deformation features have been documented across the United Kingdom, most commonly as borehole breakouts and drilling induced tensile fractures (DIFs). Recent studies using borehole imaging have allowed more detailed investigation of these features and the processes that control their formation. Within the Pennsylvanian Pennine Coal Measures Group (PCM) of the United Kingdom borehole imaging has highlighted a disproportionately high number of breakouts occurring within paleosols located immediately below coal seams. To understand the processes controlling breakout formation, a 10.5 m section of core from the Melbourne 1 borehole, incorporating a typical coal seam / paleosol sequence, was analyzed using multiple techniques including: scanning electron and optical microscopy, X-Ray Fluorescence (XRF), X-ray radiography, Point Load testing, wireline petrophysics and track-based core scanning for physical properties. Strength measurements highlight that breakouts form preferentially in poorly consolidated sediments, with low tensile strength, cross-cut by listric surfaces. The formation and termination of breakouts also corresponds to zones of diagenetic iron mineral growth with a lower propensity to fail. These coincide with greater preservation of sedimentary structures and an increase in the rock’s tensile strength; this intra-unit variation in tensile strength constrains breakout length. This demonstrates that secondary diagenetic processes, including the growth of iron minerals impose, lithological controls on the formation and length of borehole breakouts within the United Kingdom PCM.
Item Type: | Publication - Article |
---|---|
Digital Object Identifier (DOI): | 10.3389/feart.2019.00163 |
Additional Keywords: | borehole breakouts, lithology, failure, deformation, core scanning, petrography |
NORA Subject Terms: | Earth Sciences |
Date made live: | 02 Jul 2019 10:35 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/524099 |
Actions (login required)
View Item |
Document Downloads
Downloads for past 30 days
Downloads per month over past year