Poster #125, Stress and Deformation Over Time (SDOT)
Reconciling crustal stress heterogeneity from borehole breakouts and earthquake focal mechanisms
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Poster Presentation
2020 SCEC Annual Meeting, Poster #125, SCEC Contribution #10639 VIEW PDF
onding SHmax probability distributions, then compared with the associated borehole breakout-derived estimate. We find good agreement when both methods sample the basement stress (breakouts are close to the sediment-basement interface), or when both methods sample the mid-basin stress (sufficient earthquakes are present within a sedimentary basin). Along sedimentary basin margins, in contrast, we find acceptable agreement only when focal mechanisms are limited to shallow and close earthquakes, implying short-length-scale heterogeneity of < 20 km. While the region as a whole shows evidence of both lateral and vertical stress orientation heterogeneity, we find a more homogeneous stress state within basement rock, over length scales of 1 – 35 km. These results reconcile the apparently conflicting observations of short-length-scale heterogeneity observed in boreholes, which sample primarily the basins, with the relative homogeneity of stress inferred from focal mechanisms, which sample primarily the basement, and imply distinct regimes for the appropriate use of each type of stress indicator.
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