2014
DOI: 10.1016/j.ijrmms.2014.07.001
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Impact of fracture networks on borehole breakout heterogeneities in crystalline rock

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Cited by 30 publications
(33 citation statements)
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“…However, stress rotations of 20° or more are frequently observed locally in borehole data. Such rotations can be explained by slip on faults and reflect the heterogeneity of the state of stress (Barton and Zoback, 1994;Sahara et al, 2014;Schoenball and Davatzes, 2017).…”
Section: Retrospective Estimations Of Fspmentioning
confidence: 99%
“…However, stress rotations of 20° or more are frequently observed locally in borehole data. Such rotations can be explained by slip on faults and reflect the heterogeneity of the state of stress (Barton and Zoback, 1994;Sahara et al, 2014;Schoenball and Davatzes, 2017).…”
Section: Retrospective Estimations Of Fspmentioning
confidence: 99%
“…This theory was investigated on the basis of breakouts, identified by Sahara et al (2014). They analyzed breakouts in the deeper part of the well GPK4.…”
Section: Impacts Of Hydrothermal Alteration On Rock Mechanicsmentioning
confidence: 99%
“…They analyzed breakouts in the deeper part of the well GPK4. On Figure 4, a total of 2,440 breakouts from Sahara et al (2014) together with the SCCL for this depth interval are illustrated. A correlation between clay content and the appearance and size of the breakouts is obvious.…”
Section: Impacts Of Hydrothermal Alteration On Rock Mechanicsmentioning
confidence: 99%
“…[64] At such depths,s light variations in stress magnitude and orientation play as ignificant role.I na ddition, the deeply seated reservoir is highly fractured. Fractures are repeatedly accompanied by mineral alteration, acting as weak zones,w hich potentially promote failurea long such heterogeneities.…”
Section: Borehole Failurementioning
confidence: 99%
“…However, recent observations made in deep boreholes (see previous sections) indicate complex coupleda nd time-dependent damage or mechanisms (Figure 14), [72] as-yet undetected transient microphysical processes, [74] and the severei nfluence of local material or structural instabilities. [64] Fort hese microprocesses, naturally encountered at elevated temperatures at which EGSs are located (depth > 5km), lower deviatoric stresses and/orl onger geological timescales are requiredt oi nduce localization instabilities. [75] At this point, evenu nconventional brittlem aterial assumptionsf ail to correctly predict the rock strengthb ecause the material reveals as evere temperature and rates ensitivity.…”
Section: 18f Ailure Mechanismsand Materials Behaviormentioning
confidence: 99%