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Fig. 9 | Earth, Planets and Space

Fig. 9

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

Fig. 9

Shear strain rate changed by increased temperature for a W1E and b W30E. The broken contour lines show the shear strain rate with the temperature field of a 1-D geothermal gradient, and the solid contour lines show the shear strain rate with the temperature field from a 3 Myr simulation. Gray broken lines and solid lines represent the BDT depth at t = 0 and at t = 3Myr, respectively

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