pith. sign in

arxiv: 2604.16011 · v1 · submitted 2026-04-17 · 💻 cs.CV · cs.SD· physics.geo-ph

Breakout-picker: Reducing false positives in deep learning-based borehole breakout characterization from acoustic image logs

Pith reviewed 2026-05-10 09:20 UTC · model grok-4.3

classification 💻 cs.CV cs.SDphysics.geo-ph
keywords borehole breakoutsdeep learningacoustic image logsfalse positive reductionbreakout detectionin-situ stress analysisimage classificationazimuthal symmetry
0
0 comments X

The pith

Breakout-picker cuts false positives in deep learning detection of borehole breakouts by training on confusing non-breakout features and applying symmetry validation.

A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.

The paper presents Breakout-picker as a deep learning framework to automatically identify borehole breakouts in acoustic image logs. These breakouts appear as paired low-amplitude zones with near-symmetric azimuths and enlarged borehole radius, but prior deep learning methods frequently mislabel similar features such as fractures, keyseats, or artifacts as breakouts. Breakout-picker addresses this by adding negative training examples of those non-breakout features and by imposing an azimuthal symmetry filter that discards detections lacking the expected near-symmetry. Tests on three separate acoustic log datasets show higher accuracy and markedly lower false positive rates than other automatic approaches. Reliable breakout identification directly supports in-situ stress analysis that relies on these features.

Core claim

Breakout-picker reduces false positives in deep learning-based borehole breakout characterization through two strategies: training with negative samples of non-breakout features including natural fractures, keyseats, and logging artifacts, plus post-detection validation that excludes candidates failing azimuthal symmetry criteria.

What carries the argument

The dual mechanism of negative-sample training for discrimination between similar image features and azimuthal symmetry filtering to remove invalid detections.

If this is right

  • Breakout-picker achieves higher accuracy than other automatic methods across three datasets from different regions.
  • It produces substantially lower false positive rates while maintaining true breakout detections.
  • The improved reliability directly benefits in-situ stress analysis that depends on accurate breakout orientations and dimensions.
  • The approach demonstrates how targeted negative examples combined with a simple geometric rule can mitigate common misclassification problems in image-based geological feature detection.

Where Pith is reading between the lines

These are editorial extensions of the paper, not claims the author makes directly.

  • The same negative-sample plus symmetry-filter pattern could be tested on other symmetric or paired feature detection tasks in noisy borehole or seismic imagery.
  • Performance gains may increase if the negative sample library is expanded to cover additional artifact types encountered in field operations.
  • The hybrid deep-learning-plus-rule-based design offers a practical route to higher trust in automated geological interpretation pipelines where pure deep learning alone produces too many errors.

Load-bearing premise

The selected negative samples of non-breakout features are representative enough across varied geological conditions and logging qualities that the symmetry filter will not exclude valid breakouts.

What would settle it

Evaluation on a new acoustic image log dataset from an unseen region or logging condition in which Breakout-picker either fails to lower the false positive rate below existing methods or misses a substantial number of confirmed breakouts due to the symmetry check.

Figures

Figures reproduced from arXiv: 2604.16011 by Guangyu Wang, Xiaodong Ma, Xinming Wu.

Figure 1
Figure 1. Figure 1: Overview of the Breakout-picker framework for automatic borehole breakout characterization with reduced false positives. In the label/segmentation [PITH_FULL_IMAGE:figures/full_fig_p003_1.png] view at source ↗
Figure 2
Figure 2. Figure 2: Illustration of determining breakout parameters from the breakout segmentation image. (a) An acoustic amplitude log segment with borehole breakouts. [PITH_FULL_IMAGE:figures/full_fig_p004_2.png] view at source ↗
Figure 3
Figure 3. Figure 3: Network architecture of Breakout-picker, which is adapted from DeepLabV3+ [17]. The backbone is replaced with ResNet-18 instead of the original [PITH_FULL_IMAGE:figures/full_fig_p005_3.png] view at source ↗
Figure 4
Figure 4. Figure 4: Examples of borehole breakouts (indicated by the blue arrows) in (a) the acoustic amplitude logs and (b) borehole radius logs from eight boreholes at [PITH_FULL_IMAGE:figures/full_fig_p006_4.png] view at source ↗
Figure 5
Figure 5. Figure 5: Breakout annotation workflow based on acoustic amplitude and borehole radius logs. The example is taken from borehole ST2. Breakout masks [PITH_FULL_IMAGE:figures/full_fig_p007_5.png] view at source ↗
Figure 6
Figure 6. Figure 6: Non-breakout areas in acoustic image logs that share similar features with breakouts. (a) Low-amplitude logging artifacts in CB2, (b) keyseats in [PITH_FULL_IMAGE:figures/full_fig_p008_6.png] view at source ↗
Figure 7
Figure 7. Figure 7: Illustration of sample augmentation used to increase the size and diversity of the training dataset. (a) An original sample from borehole CB2, including [PITH_FULL_IMAGE:figures/full_fig_p009_7.png] view at source ↗
Figure 8
Figure 8. Figure 8: Qualitative comparison of breakout segmentation results between MMDC-UNet and Breakout-picker. (a – c) Results from CB1 and (d – f) from [PITH_FULL_IMAGE:figures/full_fig_p010_8.png] view at source ↗
Figure 9
Figure 9. Figure 9: Comparison of breakout azimuths determined using different methods for (a) CB1 and (b) ST1. Red and blue circles denote manually and automatically [PITH_FULL_IMAGE:figures/full_fig_p012_9.png] view at source ↗
Figure 10
Figure 10. Figure 10: Examples showing the effect of applying the breakout validation criteria. (a) False breakout detections over a keyseat are completely removed. (b) [PITH_FULL_IMAGE:figures/full_fig_p013_10.png] view at source ↗
Figure 11
Figure 11. Figure 11: Comparison of breakout widths estimated by different automatic methods with manual measurements for borehole CB1 and ST1. For Breakout-picker, [PITH_FULL_IMAGE:figures/full_fig_p014_11.png] view at source ↗
Figure 12
Figure 12. Figure 12: Automatic breakout characterization results for the Hunt Well. (a) Comparison of breakout azimuths using Peak Detection, MMDC-UNet, and [PITH_FULL_IMAGE:figures/full_fig_p015_12.png] view at source ↗
Figure 13
Figure 13. Figure 13: Automatic breakout characterization results for Integrated Ocean Drilling Program (IODP) Hole 1256D. (a) Comparison of manually and automatically [PITH_FULL_IMAGE:figures/full_fig_p016_13.png] view at source ↗
read the original abstract

Borehole breakouts are stress-induced spalling on the borehole wall, which are identifiable in acoustic image logs as paired zones with near-symmetry azimuths, low acoustic amplitudes, and increased borehole radius. Accurate breakout characterization is crucial for in-situ stress analysis. In recent years, deep learning has been introduced to automate the time-consuming and labor-intensive breakout picking process. However, existing approaches often suffer from misclassification of non-breakout features, leading to high false positive rates. To address this limitation, this study develops a deep learning framework, termed Breakout-picker, with a specific focus on reducing false positives in automatic breakout characterization. Breakout-picker reduces false positives through two strategies. First, the training of Breakout-picker incorporates negative samples of non-breakout features, including natural fractures, keyseats, and logging artifacts. They share similar characteristics with breakouts, such as low acoustic amplitude or locally enlarged borehole radius. These negative training samples enables Breakout-picker to better discriminate true breakouts and similar non-breakout features. Second, candidate breakouts identified by Breakout-picker are further validated by azimuthal symmetry criteria, whereby detections that do not exhibit the near-symmetry characteristics of breakout azimuth are excluded. The performance of Breakout-picker is evaluated using three acoustic image log datasets from different regions. The results demonstrate that Breakout-picker outperforms other automatic methods with higher accuracy and substantially lower false positive rates. By reducing false positives, Breakout-picker enhances the reliability of automatic breakout characterization from acoustic image logs, which in turn benefits in-situ stress analysis based on borehole breakouts.

Editorial analysis

A structured set of objections, weighed in public.

Desk editor's note, referee report, simulated authors' rebuttal, and a circularity audit. Tearing a paper down is the easy half of reading it; the pith above is the substance, this is the friction.

Referee Report

3 major / 1 minor

Summary. The manuscript introduces Breakout-picker, a deep learning framework for automatic characterization of borehole breakouts from acoustic image logs. It addresses high false positive rates in existing methods by incorporating negative samples of non-breakout features (natural fractures, keyseats, logging artifacts) during training and applying an azimuthal symmetry filter to candidate detections. The authors claim that this dual strategy yields higher accuracy and substantially lower false positive rates than other automatic methods when evaluated on three acoustic image log datasets from different regions.

Significance. If the performance claims are substantiated with quantitative metrics and generalizability tests, the work would offer a practical improvement in automated breakout detection, reducing labor-intensive manual picking and enhancing the reliability of in-situ stress analysis derived from borehole breakouts in geomechanics and petroleum engineering applications.

major comments (3)
  1. Abstract: The central claim that Breakout-picker 'outperforms other automatic methods with higher accuracy and substantially lower false positive rates' is unsupported by any numerical metrics, error bars, dataset sizes, baseline comparisons, or implementation details, leaving the primary performance assertion without verifiable evidence in the text.
  2. Methods (negative sample and symmetry filter description): The selection and diversity of negative training samples (fractures, keyseats, artifacts) and the precise definition/thresholds of the azimuthal symmetry criteria are not specified with quantitative details, ablation results, or tests for representativeness across logging qualities and geologies; this directly bears on whether the claimed FP reduction generalizes.
  3. Results (evaluation on three regional datasets): No ablation studies isolating the contribution of negative sampling versus the symmetry filter, nor cross-validation or error analysis, are reported, making it impossible to confirm that the strategies are load-bearing for the accuracy and FP improvements asserted.
minor comments (1)
  1. The abstract would be strengthened by including at least one key quantitative result (e.g., accuracy or FP rate delta) to allow readers to gauge the magnitude of improvement without reading the full results section.

Simulated Author's Rebuttal

3 responses · 0 unresolved

We thank the referee for their constructive feedback. We address each major comment point by point below, indicating revisions where the manuscript will be strengthened.

read point-by-point responses
  1. Referee: Abstract: The central claim that Breakout-picker 'outperforms other automatic methods with higher accuracy and substantially lower false positive rates' is unsupported by any numerical metrics, error bars, dataset sizes, baseline comparisons, or implementation details, leaving the primary performance assertion without verifiable evidence in the text.

    Authors: We agree that the abstract, being a concise summary, lacks the specific numerical support needed for immediate verification of the performance claims. The full manuscript contains quantitative evaluations on three datasets with accuracy and false-positive comparisons to baselines. We will revise the abstract to incorporate key metrics (accuracy, FP reductions), dataset sizes, and brief baseline references so the central claim is substantiated directly in the abstract. revision: yes

  2. Referee: Methods (negative sample and symmetry filter description): The selection and diversity of negative training samples (fractures, keyseats, artifacts) and the precise definition/thresholds of the azimuthal symmetry criteria are not specified with quantitative details, ablation results, or tests for representativeness across logging qualities and geologies; this directly bears on whether the claimed FP reduction generalizes.

    Authors: We acknowledge that the Methods section would benefit from greater quantitative specificity. We will expand it to detail the number and selection criteria for negative samples by category, their distribution across logging conditions, the exact azimuthal symmetry thresholds (e.g., azimuth deviation limit and symmetry score), and any representativeness checks using the three regional datasets. We will also add ablation results quantifying the contribution of negative sampling and the symmetry filter to FP reduction. revision: yes

  3. Referee: Results (evaluation on three regional datasets): No ablation studies isolating the contribution of negative sampling versus the symmetry filter, nor cross-validation or error analysis, are reported, making it impossible to confirm that the strategies are load-bearing for the accuracy and FP improvements asserted.

    Authors: We recognize that the Results section reports overall performance but omits ablations and supporting analyses. We will add ablation experiments isolating negative-sample training and the symmetry filter, together with cross-validation details and per-dataset error analysis, to demonstrate that these components drive the observed accuracy and FP improvements. revision: yes

Circularity Check

0 steps flagged

No circularity; standard supervised training plus domain-knowledge filter

full rationale

The paper presents a conventional deep-learning pipeline: a model is trained on labeled breakouts plus explicitly chosen negative examples (fractures, keyseats, artifacts) that share amplitude/radius traits, then a post-hoc filter discards detections lacking the azimuthal symmetry already stated in the problem definition. No equations, fitted parameters, or self-citations are shown to redefine the target quantity or force the reported accuracy gains. Evaluation is performed on three separate regional datasets, and the symmetry criterion is an independent physical property rather than a learned or self-referential construct. No load-bearing self-citation chains, ansatz smuggling, or renaming of known results appear in the provided text.

Axiom & Free-Parameter Ledger

0 free parameters · 2 axioms · 0 invented entities

The central claim rests on two domain assumptions about breakout appearance and the sufficiency of negative examples; no new physical entities or free parameters are introduced in the abstract.

axioms (2)
  • domain assumption Negative samples of natural fractures, keyseats, and logging artifacts share low-amplitude or enlarged-radius traits with breakouts yet remain distinguishable by a trained model.
    Invoked to justify the first training strategy.
  • domain assumption True breakouts exhibit near-symmetry in azimuth.
    Invoked to justify the post-detection validation filter.

pith-pipeline@v0.9.0 · 5597 in / 1437 out tokens · 51442 ms · 2026-05-10T09:20:08.921579+00:00 · methodology

discussion (0)

Sign in with ORCID, Apple, or X to comment. Anyone can read and Pith papers without signing in.

Reference graph

Works this paper leans on

40 extracted references · 40 canonical work pages

  1. [1]

    Northeast-southwest compressive stress in alberta evidence from oil wells,

    J. S. Bell and D. I. Gough, “Northeast-southwest compressive stress in alberta evidence from oil wells,”Earth and Planetary Science Letters, vol. 45, no. 2, pp. 475–482, 1979

  2. [2]

    Orientation of the stress field from breakouts in a crystalline well in a seismic active area,

    P. Bl ¨umling, K. Fuchs, and T. Schneider, “Orientation of the stress field from breakouts in a crystalline well in a seismic active area,”Physics of the Earth and Planetary Interiors, vol. 33, no. 4, pp. 250–254, 1983

  3. [3]

    Well bore breakouts and in situ stress,

    M. D. Zoback, D. Moos, L. Mastin, and R. N. Anderson, “Well bore breakouts and in situ stress,”Journal of Geophysical Research: Solid Earth, vol. 90, no. B7, pp. 5523–5530, 1985

  4. [4]

    Moos and M

    D. Moos and M. D. Zoback, “Utilization of observations of well bore failure to constrain the orientation and magnitude of crustal stresses: application to continental, deep sea drilling project, and ocean drilling program boreholes,”Journal of Geophysical Research: Solid Earth, vol. 95, no. B6, pp. 9305–9325, 1990. 19

  5. [5]

    Determination of stress orientation and magnitude in deep wells,

    M. D. Zoback, C. Barton, M. Brudy, D. Castillo, T. Finkbeiner, B. Grol- limund, D. Moos, P. Peska, C. Ward, and D. Wiprut, “Determination of stress orientation and magnitude in deep wells,”International Journal of Rock Mechanics and Mining Sciences, vol. 40, no. 7-8, pp. 1049–1076, 2003

  6. [6]

    Localized rotation of principal stress around faults and fractures determined from borehole breakouts in hole b of the taiwan chelungpu-fault drilling project (tcdp),

    W. Lin, E.-C. Yeh, J.-H. Hung, B. Haimson, and T. Hirono, “Localized rotation of principal stress around faults and fractures determined from borehole breakouts in hole b of the taiwan chelungpu-fault drilling project (tcdp),”Tectonophysics, vol. 482, no. 1-4, pp. 82–91, 2010

  7. [7]

    Stress magnitudes in the basel enhanced geothermal system,

    B. Valley and K. F. Evans, “Stress magnitudes in the basel enhanced geothermal system,”International Journal of Rock Mechanics and Mining Sciences, vol. 118, pp. 1–20, 2019

  8. [8]

    Application of supervised machine learning classification models to identify borehole breakouts in carbonate reservoirs based on conventional log data,

    N. Bashmagh, W. Lin, and K. Ishitsuka, “Application of supervised machine learning classification models to identify borehole breakouts in carbonate reservoirs based on conventional log data,”International Journal of the JSRM, vol. 20, no. 1, 2024

  9. [9]

    Stress-induced borehole elongation: A comparison between the four-arm dipmeter and the borehole televiewer in the auburn geothermal well,

    R. Plumb and S. Hickman, “Stress-induced borehole elongation: A comparison between the four-arm dipmeter and the borehole televiewer in the auburn geothermal well,”Journal of Geophysical Research, vol. 90, pp. 5513–5521, 1985

  10. [10]

    Subsurface fracture analysis and determination of in-situ stress direction using fmi logs: An example from the santonian carbonates (ilam formation) in the abadan plain, iran,

    M. Rajabi, S. Sherkati, B. Bohloli, and M. Tingay, “Subsurface fracture analysis and determination of in-situ stress direction using fmi logs: An example from the santonian carbonates (ilam formation) in the abadan plain, iran,”Tectonophysics, vol. 492, no. 1, pp. 192–200, 2010

  11. [11]

    Automated breakout detection current possibilities and their benefit for wellbore stability prediction,

    S. Wessling, T. Dahl, D. Pantic, and J. Pei, “Automated breakout detection current possibilities and their benefit for wellbore stability prediction,” inSPWLA 52nd Annual Logging Symposium, vol. All Days, SPWLA-2011-T, Conference Proceedings

  12. [12]

    Automated borehole breakout interpretation from ultrasonic imaging: Application to a deep borehole drilled into the crystalline crust,

    W. Wang and D. Schmitt, “Automated borehole breakout interpretation from ultrasonic imaging: Application to a deep borehole drilled into the crystalline crust,” inARMA US Rock Mechanics/Geomechanics Symposium. ARMA, Conference Proceedings, pp. ARMA–2020–1270

  13. [13]

    Automatic detection of fractures and breakouts patterns in acoustic borehole image logs using fast-region convolutional neural networks,

    L. O. Dias, C. R. Bom, E. L. Faria, M. B. Valent ´ın, M. D. Correia, M. P. de Albuquerque, M. P. de Albuquerque, and J. M. Coelho, “Automatic detection of fractures and breakouts patterns in acoustic borehole image logs using fast-region convolutional neural networks,” Journal of Petroleum Science and Engineering, vol. 191, p. 107099, 2020

  14. [14]

    Automatic detection of borehole breakout for image logs using yolo algorithm,

    J. Yeom, H. Kim, C. Chang, Y . Jo, Z. Chen, and K. Lee, “Automatic detection of borehole breakout for image logs using yolo algorithm,” Geoenergy Science and Engineering, vol. 252, p. 213925, 2025

  15. [15]

    Automated extraction of bore- hole breakout properties from acoustic televiewer (atv) data,

    J. Yang, S. Goodfellow, and J. Harrison, “Automated extraction of bore- hole breakout properties from acoustic televiewer (atv) data,” inARMA US Rock Mechanics/Geomechanics Symposium. ARMA, Conference Proceedings, pp. ARMA–2022–0408

  16. [16]

    A semi-supervised approach for borehole image log structures segmentation for small labeled datasets,

    A. D. Cunha, G. B. D. Anjos, R. Nascimento, C. M. de Jesus, and J. Jauregui, “A semi-supervised approach for borehole image log structures segmentation for small labeled datasets,” vol. 2025, no. 1, pp. 1–5, 2025

  17. [17]

    Encoder- decoder with atrous separable convolution for semantic image segmen- tation,

    L.-C. Chen, Y . Zhu, G. Papandreou, F. Schroff, and H. Adam, “Encoder- decoder with atrous separable convolution for semantic image segmen- tation,” inProceedings of the European conference on computer vision (ECCV), 2018, Conference Proceedings, pp. 801–818

  18. [18]

    Stress concentration at the bottom of a borehole and its effect on borehole breakout formation,

    T. Ito, K. Kurosawa, and K. Hayashi, “Stress concentration at the bottom of a borehole and its effect on borehole breakout formation,”Rock Mechanics and Rock Engineering, vol. 31, no. 3, pp. 153–168, 1998

  19. [19]

    Micromechanisms of borehole instability leading to break- outs in rocks,

    B. Haimson, “Micromechanisms of borehole instability leading to break- outs in rocks,”International Journal of Rock Mechanics and Mining Sciences, vol. 44, no. 2, pp. 157–173, 2007

  20. [20]

    Evolution of stress-induced borehole breakout in inherently anisotropic rock: Insights from discrete element modeling,

    K. Duan and C. Y . Kwok, “Evolution of stress-induced borehole breakout in inherently anisotropic rock: Insights from discrete element modeling,”Journal of Geophysical Research: Solid Earth, vol. 121, no. 4, pp. 2361–2381, 2016

  21. [21]

    Impact of fracture networks on borehole breakout heterogeneities in crystalline rock,

    D. P. Sahara, M. Schoenball, T. Kohl, and B. I. M ¨uller, “Impact of fracture networks on borehole breakout heterogeneities in crystalline rock,”International Journal of Rock Mechanics and Mining Sciences, vol. 71, pp. 301–309, 2014

  22. [22]

    Multi-disciplinary characterizations of the bedrettolab – a new underground geoscience research facility,

    X. Ma, M. Hertrich, F. Amann, K. Br ¨oker, N. Gholizadeh Doonechaly, V . Gischig, R. Hochreutener, P. K¨astli, H. Krietsch, M. Marti, B. N ¨ageli, M. Nejati, A. Obermann, K. Plenkers, A. P. Rinaldi, A. Shakas, L. Vil- liger, Q. Wenning, A. Zappone, F. Bethmann, R. Castilla, F. Seberto, P. Meier, T. Driesner, S. Loew, H. Maurer, M. O. Saar, S. Wiemer, and ...

  23. [23]

    Fault zone spatial stress variations in a granitic rock mass: Revealed by breakouts within an array of boreholes,

    S. Zhang, X. Ma, K. Br ¨oker, R. van Limborgh, Q. Wenning, M. Hertrich, and D. Giardini, “Fault zone spatial stress variations in a granitic rock mass: Revealed by breakouts within an array of boreholes,”Journal of Geophysical Research: Solid Earth, vol. 128, no. 8, p. e2023JB026477, 2023

  24. [24]

    Borehole image log and statistical analysis of foh-3d, fallon naval air station, nv,

    K. Blake and N. C. Davatzes, “Borehole image log and statistical analysis of foh-3d, fallon naval air station, nv,” inProceedings of the thirty-seventh workshop on geothermal reservoir engineering, 2012, Conference Proceedings

  25. [25]

    Structural interpretation from televiewer surveys,

    R. Thomas, J. Neilsen, H. Wilson, and P. Lamb, “Structural interpretation from televiewer surveys,” inFMGM 2015: Proceedings of the Ninth Symposium on Field Measurements in Geomechanics. Australian Centre for Geomechanics, 2015, pp. 729–741

  26. [26]

    In-situ stress orientation and magnitude at the fenton geothermal site, new mexico, determined from wellbore breakouts,

    C. A. Barton, M. D. Zoback, and K. L. Burns, “In-situ stress orientation and magnitude at the fenton geothermal site, new mexico, determined from wellbore breakouts,”Geophysical Research Letters, vol. 15, no. 5, pp. 467–470, 1988

  27. [27]

    Estimation of maximum horizontal principal stress magnitude from stress-induced well bore breakouts in the cajon pass scientific research borehole,

    L. Vernik and M. D. Zoback, “Estimation of maximum horizontal principal stress magnitude from stress-induced well bore breakouts in the cajon pass scientific research borehole,”Journal of Geophysical Research: Solid Earth, vol. 97, no. B4, pp. 5109–5119, 1992

  28. [28]

    Subsurface geophysical characterization of the crystalline canadian shield in northeastern alberta: implications for geothermal development,

    J. S. Chan, “Subsurface geophysical characterization of the crystalline canadian shield in northeastern alberta: implications for geothermal development,” Ph.D. dissertation, University of Alberta, 2013

  29. [29]

    Iodp expeditions 309 and 312 drill an intact section of upper oceanic basement into gabbros,

    J. C. Alt, D. A. H. Teagle, S. Umino, S. Miyashita, N. R. Banerjee, D. S. Wilson, I. E. the, Scientists, and O. D. P. L. S. P. the, “Iodp expeditions 309 and 312 drill an intact section of upper oceanic basement into gabbros,”Sci. Dril., vol. 4, pp. 4–10, 2007

  30. [30]

    Heterogeneity versus anisotropy and the state of stress in stable cratons: Observations from a deep bore- hole in northeastern alberta, canada,

    W. Wang, D. R. Schmitt, and J. Chan, “Heterogeneity versus anisotropy and the state of stress in stable cratons: Observations from a deep bore- hole in northeastern alberta, canada,”Journal of Geophysical Research: Solid Earth, vol. 128, no. 3, p. e2022JB025287, 2023

  31. [31]

    Drilling to gabbro in intact ocean crust,

    D. S. Wilson, D. A. H. Teagle, J. C. Alt, N. R. Banerjee, S. Umino, S. Miyashita, G. D. Acton, R. Anma, S. R. Barr, A. Belghoul, J. Carlut, D. M. Christie, R. M. Coggon, K. M. Cooper, C. Cordier, L. Crispini, S. R. Durand, F. Einaudi, L. Galli, Y . Gao, J. Geldmacher, L. A. Gilbert, N. W. Hayman, E. Herrero-Bervera, N. Hirano, S. Holter, S. Ingle, S. Jian...

  32. [32]

    Q. C. Wenning, T. Berthet, M. Ask, A. Zappone, J.-E. Rosberg, and B. S. G. Almqvist, “Image log analysis of in situ stress orientation, breakout growth, and natural geologic structures to 2.5 km depth in central scandinavian caledonides: Results from the cosc-1 borehole,” Journal of Geophysical Research: Solid Earth, vol. 122, no. 5, pp. 3999– 4019, 2017

  33. [33]

    Shallow tectonic stress magnitudes at the hikurangi subduction margin, new zealand,

    E. Behboudi, D. D. McNamara, and I. Lokmer, “Shallow tectonic stress magnitudes at the hikurangi subduction margin, new zealand,”Geo- chemistry, Geophysics, Geosystems, vol. 24, no. 10, p. e2022GC010836, 2023

  34. [34]

    State of stress across major faults in the nankai subduction zone estimated from wellbore breakouts,

    K. E. Schaible and D. M. Saffer, “State of stress across major faults in the nankai subduction zone estimated from wellbore breakouts,” Journal of Geophysical Research: Solid Earth, vol. 130, no. 7, p. e2024JB030242, 2025

  35. [35]

    Global crustal stress pattern based on the world stress map database release 2008,

    O. Heidbach, M. Tingay, A. Barth, J. Reinecker, D. Kurfeß, and B. M ¨uller, “Global crustal stress pattern based on the world stress map database release 2008,”Tectonophysics, vol. 482, no. 1, pp. 3–15, 2010

  36. [36]

    Training region-based object detectors with online hard example mining,

    A. Shrivastava, A. Gupta, and R. Girshick, “Training region-based object detectors with online hard example mining,” inProceedings of the IEEE conference on computer vision and pattern recognition, Conference Proceedings, pp. 761–769

  37. [37]

    Hard negative examples are hard, but useful,

    H. Xuan, A. Stylianou, X. Liu, and R. Pless, “Hard negative examples are hard, but useful,” ser. Computer Vision – ECCV 2020. Springer International Publishing, Conference Proceedings, pp. 126–142

  38. [38]

    Borehole logging data (acoustic and optical televiewer) from boreholes in the bedretto lab [dataset],

    K. E. N. Br ¨oker, Q. Wenning, M. Hertrich, and X. Ma, “Borehole logging data (acoustic and optical televiewer) from boreholes in the bedretto lab [dataset],” 2023. [Online]. Available: https: //doi.org/10.3929/ethz-b-000616727

  39. [39]

    Geophysical logging and image data from the hunt well, ne alberta [dataset],

    D. Schmitt, W. Wang, and J. Chan, “Geophysical logging and image data from the hunt well, ne alberta [dataset],” 2022. [Online]. Available: https://doi.org/10.5683/SP3/YYNVW8

  40. [40]

    Acoustic image log borehole breakout dataset for advancing deep learning in automatic breakout characterization from image logs,

    G. Wang, “Acoustic image log borehole breakout dataset for advancing deep learning in automatic breakout characterization from image logs,” Feb. 2026. [Online]. Available: https://doi.org/10.5281/zenodo.18627151