Quantifying sand delivery to deep water during changing sea‐level: Numerical models from the Quaternary Brazos Icehouse continental margin

Sequence stratigraphy for clastic continental margins predicts the development of sand‐rich turbidite deposits during specific times in relation to base‐level cycles. It is now widely understood that deltas can extend to the shelf‐edge forced by high sediment flux and/or base level, providing a dire...

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