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The correlation lengths measured from the wide angle reflections are in the range of 80±10 Å for all the polymers except for ASP-5 (∼40 Å).
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The OUC is crossed by recently acquired WARR (wide angle reflection and refraction) PANCAKE profile (Starostenko et al., 2013).
The X-ray patterns of all ATPs and ASPs studied show a series of ordered reflections in the small angle region and a sharp wide angle reflection at d=∼4.4 Å, characteristic of a smectic phase.
The d-spacing of the wide angle reflection, 4.4 Å, suggests that paraffinic side chain crystallization does not occur and that the smectic mesophase develops through dipole dipole interactions of sulfone groups in the side chains.
Both the correlation length (from the wide angle reflection) and the layer thickness decreased from ∼80 to ∼30 Å and from 46 to 40 Å at this transition, respectively, indicating that the order in the smectic layers is lost and the SB structure has become a less ordered SA structure at this transition.
My adviser asked me if I would be interested in looking at these wide-angle reflections that had been observed in the data.
Figure 2a shows the seismic record section of SP-W1 (northernmost shot on the western profile), with the deep wide-angle reflections highlighted by a red arrow.
An effective integration of traveltime tomography, CDP reflection processing and prestack depth migration of wide-angle reflections applied to our data, allowed us to present the model in which we deduced the contact zone of the Variscan overthrust structure (Variscan front) with its molasse-filled foredeep.
Ito et al. (2006) carried out the refraction and wide-angle reflection surveys by controlled sources and found some reflectors.
My main contribution here was the addition of code that determined the geometry of a reflector surface from travel times of wide-angle reflection data.
The combination of wide-angle reflection and near-vertical reflection data has facilitated a more complete geological interpretation of the seismic data.
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