Both parameters indicate a significant reduction in recombination.
BP, the alluvial architecture and grain-size parameters indicate a wandering river.
All of these parameters indicate a direct proportionality with tarmat thickness and magnitude of pressure required to fail the tarmat.
The considerable differences in robustness across trabecular parameters indicate a need for selecting the most stable parameters, most notably for longitudinal studies of small numbers of patients.
At the same time, rock magnetic parameters indicate a preferential destruction of fine-grained magnetic particles in older paleosols resulting from seasonal excess moisture.
Both the linear and nonlinear parameters indicate a faster recovery of the baseline HRV corresponding to the preconditioned groups, though only the spectral analysis identifies a statistically significant difference between the two groups.
Finally, failure maps depending on key geometry parameters indicate a clear distinction between an out-of-plane and an in-plane buckling mode whereas the latter results in lower critical strains.
All these parameters indicate a G0 quiescent state.
