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How brittle detachments form and evolve through space and time

Figure 8. Time-constrained model for brittle detachments evolution. (A) crustal thinning, hinge rolling and brittle-ductile detachment zones initiation. (B) Deformation localisation along the main brittle detachment, gouge formation and development of SC structure-dominated shear zone, coeval with the onset of ductile deformation along the upper part of the exhuming granite.

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About the “predecessors” of the 2023 Februaryearthquakes, Turkey

Approximate epicentral areas of the major EAFZ earthquakes of the period 1000-1900, superimposed on the 2023 seismic sequence. In red the earthquakes considered in this study. The 2023 seismicity (pink circles) comes from KOERI (Kandilli Observatory and Earthquake Research Institute); http://www.koeri.boun.edu.tr/scripts/lasteq.asp). Faults traces (red lines) from www.seismofaults.eu/; Digital…

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