Features of sedimentary rocks possibly due to internal waves

Stanisław Mateusz Gąsiorowski

Abstract


Fale wewnętrzne a sedymentacja

It seems possible that internal waves may be a cause of ripple marks, graded bedding, mega-ripples, swash marks, deposition of layers of clastics, and that the associated backwash currents may leave marks similar to those left by other currents.

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