Article ID Journal Published Year Pages File Type
4689723 Sedimentary Geology 2012 14 Pages PDF
Abstract
► Internal-wave deposits (internalites) are described. ► They formed from tractive up- and down-dip flows caused by breaking internal waves. ► Stacking of internalites reflects sediment-input changes and pycnocline fluctuation. ► A depositional model for sandy-oolitic internalites in mid-ramp setting is presented. ► Criteria for differentiating internalites from tempestites are provided.
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Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
Preview
A facies model for internalites (internal wave deposits) on a gently sloping carbonate ramp (Upper Jurassic, Ricla, NE Spain)
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