fig06.htm

Figure 6. Relative numbers of earthquakes with M>3 (solid line) and M>5 (broken line) as a function of the difference between the maximum and minimum principal values of the stress tensor S1-S3 (in units of 10 MPa) calculated at a depth of 12.5 km in the Baikal rift zone. The earthquake sources of the sample are not deeper than 20 km.


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