Phase transitions in olivine may be the cause of deep seismic faulting NatureComms
). This suggests that the occurrence of a throughgoing fault slip caused by the rupture was followed by rupture propagation outside the sample. Among the three runs where faulting and blow-out occurred, one run using the upgraded X-ray detector system with the P-T-t path#3 most clearly shows the deformation processes and associated AE activities .
Notable softening of the deforming sample was observed before the occurrence of throughgoing faulting in M3425 with high time-resolution stress/strain measurements . Such softening was also accompanied by the large AEs in other runs with the P-T-t path#3 which experienced no faulting . The softening was likely to be initiated by temperature ramping ) during the sample deformation in the P-T-t path#3.
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