The colinearity measure outlined in methods (and the associated distribution of maximum orientation) provides a robust means of differentiating between forms of perimysial collagen in the cross-fiber plane (see Fig. 1).
However, industry needs a precise knowledge of the maximum orientation and position output errors at a given nominal configuration.
At locations where maximum loadings occurred, orientation of the building was changed to explore its effect on peak loads.
We argue that the maximum weight of an orientation of (T w v, P w v ) orienting the edges on path T (v, w) towards w equals (4) A (v, w ) + ∑ i = 1 ℓ max S (u i, w ), S (v, u i ) - A (v, w ), and, hence, S v, w) is computed correctly.
In the eastern Central Range of Taiwan there is a regional variation in the orientation of maximum finite stretch across the slate belt, with down-dip maximum stretch found in the western Central Range and along-strike maximum stretch in the eastern Central Range.
Observe that m a x c r ∈ C r S (r, r, c r ) is the maximum weight of an orientation of the whole instance (T, P, ω) since T r r = T and we build the maximum over all colorings of the cross pairs in Q r.
For the correctness, we argue that for v, w ∈ V with v ≺ w and for a coloring c w ∈ C w that is feasible for case (1), the maximum weight of an orientation of (T w v, P w v ) consistent with c w that orients the edges on path T (v, w) from v to w is A (v, w ) + W LCA (w, c w ) + ∑ i = 1 ℓ M (u i, v, w, c w ), and, hence, S v, w, c w) is computed correctly.
These stress orientation data suggest that the dominant orientation of maximum principal compressive stress in the Late Mesozoic is WNW.
It is suggested that the orientation of maximum horizontal stress (SHmax) relative to the Mesozoic faults, forming hydrocarbon traps, is critical for their potential seal/leak behaviour.
