Therefore, from Eq. (1), dμ/du in the second term of the right-hand side of Eq. (4) can be expressed as (6) where T+ΔTt′ denotes the unit vector in the direction of the slip increment (T+ΔTu t − T u t )/|T+ΔTu t − T u t |, as shown in Fig. 1.
Fig. 9 Maximum tendencies for slip with T S >0.6 (a) and dilation with T D >0.7 (b) of the predominant fault settings in the southern Black Forest obtained from lineament analyses of digital elevation models (LIDAR-DEM5).
S = Slip traces, T = twin bands, C = cracking, (Ref).
We refer to the afterslip as true slip (s t).
For the numerical inversion test, we calculated the true values of these hyperparameters from the true slip s t.
As the result, the measured distribution of vitrinite reflectance is reasonably fitted with heat generation rate ( left(dot{Q}right) ) and slip duration (t r ) of 16,600 J/s/m2 and 6,250 s, respectively, for the megasplay and 23,200 J/s/m2 and 2,350 s, respectively, for the frontal décollement, implying slow and long-term slips.
Regression analysis was performed to determine the relationships between each of the characteristic values of slip and t e. Linear regression analysis of 12 measurements collected at the characteristic points tested in this study yielded the best-fit line given in Eq. (6): s_{1} = 0.0086 cdot t_{e} + 6.203, (6a) s_{2} = 0.014 cdot t_{e} + 12.983, (6b) s_{3} = 0.0104 cdot t_{e} + 17.417.
Three 3/4-inch slip plastic "T" fittings.
Slip the t-shirt over your head but do not pull it past your shoulders.
Attach your suspenders to a pair of rugged jeans and slip a t-shirt or tank top on underneath.
