The results show that stiffness of an inclusion and its location have a significant effect on the RCF life: stiffer inclusions and inclusions located at the depth of maximum shear stress reversal are more detrimental to the RCF life.
The largest shear stress is located at the depth of the BDT.
In both mechanisms, the base of the lithosphere would have been located at the depth where partial melting is initiated.
The top of each layer i is located at the depth z i−1, and its bottom at depth z i = z i−1 + h i.
The purpose layer is located at the depth between 5200 and 5300 m, developed as part of the second formation of the lower Carboniferous (Kalashayi formation).
Furthermore, most of the aftershocks of the Ruisui earthquake are located at the depth range of about 6 18 km as illustrated by the relocation of events occurred over the five first days (about 800 events, see Fig. 9).
In our models, the minimum grain sizes are located at the depth of BDT under the fault where shear stress becomes the largest, nearly equal to the frictional strength of the fault.
The results of our study indicate that, after the accelerated CXL procedure, the line is located at the depth of approximately 282 μm within anterior corneal layers, similar to the standard CXL procedure [ 26].
