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| Name：Georgebex | 09, Mar, 2024 01:07:07 | |
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which ranged from above fairweather to below storm wave base. Intrinisic processes such as storm and wave redeposition and reworking may have acted to inhibit aggradation into the zone of peritidal sedimentation. Estimates of water depth during deposition range from a few metres to a few tens metre | |
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