Lecture: Shelf to Pelagic Environments

Lecture: Shelf to Pelagic Environments Clastic sediment depositional processes • Continental Shelf • Continental Slope/Rise • Deep Sea (Pelagic) Neop...
Author: Erick Parsons
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Lecture: Shelf to Pelagic Environments Clastic sediment depositional processes • Continental Shelf • Continental Slope/Rise • Deep Sea (Pelagic)

Neoproterozoic Storms

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Clastic Shelf Settings – 5% Earth covered in water < 200m deep – Palimpsest Effect- reworking of relict sediments deposited at lower sea levels – Shelf sands - high porosity & permeability

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Extent of the modern shelves

Epeiric seas: large bodies of shallow water. 75 Ma

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Current Velocity/Grain Size Influence sedimentary structure and texture – Tidal Currents: a few to >100 cm/sec, all depths – Storms: Variable 10-100 cm/sec – Geostrophic Currents: 4 m) zones • strong tide currents (>100 cm/s) - sand ribbons or ridges – up to 40 m high – km wide & long – Low angle x-strata

• weaker currents (