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Fig. 4 | Earth, Planets and Space

Fig. 4

From: Shear strain concentration mechanism in the lower crust below an intraplate strike-slip fault based on rheological laws of rocks

Fig. 4

Contours of shear stress (\(\tau _{s}\)) in the lower crust as a function of depth and distance from the fault for models a W1E, b D1E, c W30E, d W1C, e D1C, and f W30C. The thickness of the lower crust and the depth of the BDT are dependent on the assumed rheology and far-field velocity (\(v_{0}\)). The gray broken lines represent the BDT depth

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