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

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

Dec 1983

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1983pepi...33..250b&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 33, Issue 4, p. 250-254.

Physics

7

Scientific paper

The orientation of the regional stress field in the Swabian Jura was determined from borehole breakouts caused by stress accumulation at the borehole wall. The analysis is based on caliper data recorded in the Urach 3 geothermal well within an intervall of about 1450 m. The azimuths of the breakouts are consistent with depth and indicate a stress direction which is in good agreement with the interpretation of fault plane solutions of nearby earthquakes.

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