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Fig. 10 | Progress in Earth and Planetary Science

Fig. 10

From: Rheology and stress in subduction zones around the aseismic/seismic transition

Fig. 10

a Train of crenulations in pelitic schist, showing the kink-like geometry of the microfolds. b Dynamically recrystallized metachert deformed by dislocation creep, cut by a quartz vein produced by hydraulic fracture. The vein shows cross-fiber geometry, indicating the direction of opening, and grain-boundary bulging and dynamic recrystallization indicating renewed dislocation creep after emplacement

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