The lateral variation in sediment within a stratum is known as sedimentary facies.
2.
The Late Eocene reflects more frequent lateral variations of interbedded limestones, dolomites, marls, and shales.
3.
This behaviour has been reproduced by modelling the viscoelastic response of the megathrust fault plane with lateral variations in both convergence rate and frictional properties.
4.
This behavior has been reproduced by modeling the viscoelastic response of the megathrust fault plane with lateral variations in both convergence rate and frictional properties.
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