380 likes | 490 Views
Sedimentary structures commonly found in deep-marine environments (continental margin). Sediment gravity flow deposits—. turbidity flows. Right-side-up or upside-down?. upside-down. Right-side-up or upside-down?. right-side-up. Torres del Paine, Chile. Point Lobos, CA. 10 cm.
E N D
Sedimentary structures commonly found in deep-marine environments(continental margin)
Sediment gravity flow deposits— turbidity flows
Right-side-up or upside-down? upside-down
Right-side-up or upside-down? right-side-up
10 cm Low-density flows
Sediment-gravity flow deposits— debris flows
Clast imbrication—long axis perpendicular to flow (in a river)
Erosion into underlying beds Sole marks—flutes
Sole marks load casts
Secondary sedimentary structures formed after deposition (sometimes only a short time after) Fluid escape structures (flames)
Convoluted beds (syn-sedimentary folds) Pigeon Point, CA
Escape structures Bioturbation in shallow water Ophiomorpha Skolithos
Opiomorpha (Ichnofacies Skolithus)
Foraging trails Bioturbation in deep water