Features of sedimentary rocks possibly due to internal waves
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.
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.