Titlebook: Stress in the Earth; Max Wyss Book 1977 Springer Basel AG 1977 Geophysik.Physik.Stress

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Stress and Shear Fracture (Fault) Patterns Resulting from a Suite of Complicated Boundary Conditiontating elastic beam subjected to boundary stresses. The boundary conditions investigated are more complicated than those previously published and include cases with sawtooth-, step-, and sinusoidally-shaped lower-boundary loads, with and without additional tectonic end loads. Potential shear fractur

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Preliminary Stress Measurements in Central California Using the Hydraulic Fracturing Technique,, and Menlo Park, California are described in detail. In the Livermore well, four measurements at depths between 110 and 155 m indicate that the least principal compressive stress is horizontal and increases from 1.62 to 2.66 MPa. The apparent direction of maximum compression is N 70° E (±40°). At t

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Crustal Stress in Iceland,flank of the Reykjanes—Langjökull continuation of the Mid-Atlantic Ridge. The measurements indicate a dominant orientation of σ. approximately perpendicular to the axial rift zone, in contrast to earthquake focal mechanism solutions from within the axial rift zone of the Reykjanes Peninsula. In one