Platform-Interior Carbonate Depositional Environments
Robert G. Loucks, Charles Kerans, and Xavier Janson
Bureau of Economic Geology
 
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Barrier Island Depositional Environments

 

The system can be divided into several environments:

(1) Beach: This includes sediments from the shore face, fore shore, and back beach.

(2) Eolian Dune: Well-developed eolian sand dunes commonly develop landward of the back beach.

(3) Tidal Channel Facies: Tidal channels commonly dissect barrier islands. Channels can contain mud-free to muddy sand depending on their depth, tidal current energy, and density of sea-grass growth.

(4) Sand Spit Facies: Sand spits can accrete laterally into tidal channels on barrier islands.

(5) Flood-Delta Facies: As tides and storms force water through tidal channels, deltas form on the flood end of the channel. These deposits range from sandy facies with isolated corals and red algae to a muddy facies with sea grass.

(6) Ebb-Delta Facies: As tides and storm waters drain back out through tidal channels, deltas form on the ebb end of the channel and produce sandy facies with corals and red algae.


Flood Delta: Florida Keys
Flood Delta: Belize
Shallow Water Spit
 
 

Click on cross-section lines to see feature cross-section.
Click on thumbnails to see example photographs.

 

 


Rock Types

Most of the rock types associated with barrier systems are crossbedded grainstones to mud-poor packstones, except where tidal flats develop behind the barrier. See section on beach, eolian dune, and tidal-flat environments for ancient examples.

 

 

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