The Interplay Between Sediment Supply, Subsidence, and Basin Fill
Size and denudation characteristics of land areas delivering terrigenous sediments.
Areal extent and geometry of corresponding basin.
Tectonic subsidence of basin floor and compaction of sediments.
Hydraulic regime of a river system or a water-filled basin.
Eustatic sea level changes.
General rules for autochthonous sediment production, including carbonate buildups.
KeywordsClay Sedimentation Compaction Sponge Dolomite
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