Intermediate and final products were characterized by 1H NMR spectroscopy, transmission electron microscopy, two-dimensional chromatography and statistical calculations, with a focus on the pivotal stage of phase inversion during the polymerisation where the salami domains are born.
The bore fluids were specially designed to vary the solvent nonsolvent exchange rates in the phase inversion stage by mixing different polymer solvent 1-methyl-2-pyrrolidinone NMPP) content inside the water or ethanol internal coagulant.
As a final step in the geophysical modeling presented here, we performed a second stage of inversion modeling to further reduce the misfit.
During the late stage of inversion, 35 min to 45 min after its onset, the last third of the anterior hemisphere moves over the already inverted cell monolayer.
During this last stage of inversion, the remaining disc-shaped cells of the not yet inverted portion of the anterior hemisphere become pencil-shaped and simultaneously seem to move over the rim of the remaining portion of the anterior cap.
Moreover, we determined the locations of CBs for each cell shape, particularly in relation to the chloroplast-end-to-flagellar-end axis, and we established consensus curvatures of the cell monolayer throughout all stages of inversion using LM, cLSM and SEM images.
Inversion progresses during the mid-inversion stage, and the CBs localize in spindle-, paddle- and disc-shaped cells just as described for the early inversion stage.
A second stage of topographic inversion occurred during the Oligocene or later.
The gates utilize a single SOA and it needs neither an inversion stage nor an additional synchronized clock.
This inversion stage is the best expressed in the field and caused dextral strike-slip faulting along the fault systems that now control the major rift structures.
