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Saturday, April 3, 2010

Sedimentary Structures

some kinds of sedimentary structures:

1. Deformational Structures

- Load cast: are rounded or bulbous protrusions formed during compaction. Where these grooves and depressions become filled with sediment, especially if the surface is mud, the marks may be preserved.
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- Convolute Bedding: appears as highly contorted, folded and disrupted layers.


- flame structure: deformed clay or silt laminations with curved, pointed ends that project into the overlying bed and resemble a flame blown in the wind.


2. Current Flow Structures

- Parallel Lamination : (where the upper and lower contacts are approximately parallel) can result from
  • settling from suspension
  • deposition in a low energy environment
  • laminar flow (water flowing in a planar way)

- Ripple Marks : formed when the current flow energy increases.


- Cross Bedding : continuous erosion of the stoss side of the ripples and deposition on the leeward side causes

- Graded Bedding: As sediment is carried from a high energy environment into a low-energy environment, the heaviest particles will be the first to settle out, followed by progressively lighter and lighter particles.



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