By applying the reflection strength attribute on the previous seismic section in Fig. 8a, sandy beds with high reflection strength (light colour) can clearly be observed enclosed by shales with low reflection strength (grey colour) (Fig. 8b).
Therefore, applying the reflection FT-IR technique to small natural samples such as melt inclusions requires developing a method to correct for spectral overlap of the signal from host minerals.
The number of observations after applying the reflection selection criteria for merging and outlier rejections for this 1.35 Å data set is 1,136,447 (∼96% of the total observed reflections).
We apply the Lambertian reflection property to the buildings, poles, cars, and road lines in order to provide a more realistic scene.
Except when (theta_{0}=0) or (pmpi /2), this would have the effect of breaking the reflection symmetry of θ, because applying the new reflection would not preserve the lattice.
By applying the Schwarz reflection principle [8], p.68, to (h'(L)), it follows that there is a function harmonic on (mathcal{T}_{n}) satisfying (h(L^)=-h'(L =-(h(L -mathbb{H}_{[tau(vert y'vert )+varpi],n}(L -mathbb{Lin overline{T}_{n}), wH}_e ∗ denotes reflection in (partialmathcal{[tau vertust as (L^=(x', -x_{n})).
The acceleration waveforms of the virtual middle-size earthquake are calculated on the engineering bedrock with an S-wave velocity of greater than or equal to 600 m/s by applying the multiple reflection theory to the acceleration waveforms, which are simulated on the seismic bedrock.
Thus, the dual form of (1) includes the constant which reduces to L ∗ ⋅ Γ Γ ( − β + m ) = π sin s π p ⋅ Γ ( s q ) Γ ( s ) Γ ( m + 1 − s p ), after applying the Euler reflection formula Γ ( x ) Γ ( 1 − x ) = π sin x π.
For indexing the different mesophases and calculating the corresponding unit lattice parameter a, we applied the respective reflection laws for the cubic and the hexagonal phases [8].
After these iterative refinement cycles are complete, we apply the refined parameters to the reflection intensities of each still, and then merge the same reduced Miller indices (from all stills) to obtain the zero-offset still intensities, which are used for the new reference intensity set (see next section).
