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At the 20-somite stage, migratory adaxial cells begin their lateral migration, and we noticed that some of these migrating adaxial cells expressed AChR clusters (Figure 1B3 B4).
But in later stages, because of rising sea level, incision abates while aggradation and lateral migration enhances, resulting in inconspicuous incised valleys.
The PEEFs are partially sealing with a lateral migration component.
After that, a tendency to lateral migration and local braiding were observed in the deepened channel.
Lateral migration is horizontal, with the thickness of sand bodies similar to that of single channel.
As the slope becomes steep, the downcutting enhances while lateral migration weakens.
Lateral migration causes sand body distribution more continuous, which expands the connected range of sand bodies.
Source-proximal hydrocarbon accumulation thus dominates without long-distance vertical and lateral migration.
The downcutting capacity of the channel weakens while the vertical and lateral migration strengthened gradually.
Here the single channel shows lateral migration, as a weakly restricted channel, and thus widely distributed.
Lateral migration and vertical downcutting are both strong for single channels, as well as high sinuosity.
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