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b Schematic image of the depth variations in the stress field.
We attribute the variations in the stress field to temporal variations.
It should be noted that depth variations in the stress regime correlate well with depth variations in electrical resistivity of the crust.
We studied variations in the stress field around guide holes drilled during tunnel excavation to understand the mechanical mechanism by which these holes help prevent rockburst.
The combined information enabled spatial variations in the stress fields in crystallographic axes to be mapped and compared directly with microstructural features such as grains and grain boundaries.
In addition, the changes in the internal micro-structure of the specimens resulted from variations in the stress condition, were found to affect the ultrasonic velocity measurements.
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We found that variations in constriction and heterogeneity led to variations in the stress-strain relation and in the elastic modulus of the airway tissue.
We, thus, interpret that the discrepancy between the variations in the stressing rate estimated from shear wave splitting and from coda Q reflects the difference of the variation in stressing rate between the brittle upper crust and the ductile part below the brittle-ductile transition zone in the crust.
Similar variation in the stress pattern was seen in the previous studies [18, 27].
We investigated the spatial variation in the stress fields of Kyushu Island, southwestern Japan.
We then divided the period from 17 August 1999 to 10 October 1999 into time intervals of 2 weeks and investigated temporal variation in the stress tensor.
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