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The boundaries and depth of this underworld evolved with the technology, so by its 3D incarnation, the ability to pick up prostitutes and mow down civilians took on a whole new level of realism.
We used a standardised strategy for assessment of the visual field but allowing for additional vectors to be added to further evaluate the boundaries and depth of any detected area of visual field loss.
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Earthquakes are by far most common along plate boundaries and rift zones: plotting the location of earthquakes allows seismologists to map plate boundaries and depths (click on the picture at the right to view a map of quake epicenters).
The source boundaries and depths are determined from the zero contours, and the half distance between ± π/4 contours or the distance between zero and + π/4 or − π/4 contour of TDR, respectively.
We describe an implementation that integrates these new codes with real-time algorithms for tracking stripe boundaries and determining depths.
The OCT signal intensity profiles between the air/tissue boundaries and the depths of SD maxima corresponding to the left and right vertical lines are shown in Figs. 6(a) and 6(b), respectively.
However, the adopted form of the asymptotic expansions ceases to be valid as the point of complete solidification is approached, where the displacements at the free boundary and the depth of the melt are of the same order.
Therefore, we can build a general procedure of third-order polynomial fitting every A-mode scan intensity profile in the range between the determined air/tissue boundary and the depth of SD maximum.
Here, one can see that in the A-mode scan intensity profile of the small discrepancy between the EP/LP boundary and the depth of SD maximum (see Fig. 6(b)), the signal intensity fluctuations are relatively weaker, when compared with those in the A-mode scan intensity profile of large discrepancy (see Fig. 6(a)).
This improvement was attributed to the integrity of coating/substrate interface without any signs of delamination, crack initiation from the surface instead of the interface, crack propagation mainly by transcrystalline mechanism and not through particle boundaries and finally high depth of compressive residual stresses.
When considering the same longitudinal and latitudinal extents for both the outer boundary and mid-depth patches, a root (at mid-depth) of an intense flux patch (at the CMB) would exhibit an apparent distortion due to the difference between the corresponding CMB and mid-depth areas of equal angular extents.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com