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- W2121998052 abstract "ABSTRACT In Alabama, Upper Cretaceous depositional sequence stratigraphy has been strongly affected by second-, third-, and fourth-order changes of sea level. In the upper Santonian to uppermost Maastrichtian section (85 to 67 Ma), second- and third-order sea-level changes owing to eustacy and third- and fourth-order sea-level changes owing to both local and regional tectonic events are recognized. Effects of second-order eustatic change are gross changes in depositional strike and systematic variations maximum clastic sedimentation rate. Effects of third-order eustatic change and local and regional tectonic events are related to directly to depositional sequence development. Fourth-order depositional sequences (episodic parasequences) are related to regional tectonic events. Tectonically affected depositional sequences are delineated by chronocorrelation with independently verified and dated local and regional (plate-wide) episodes of disturbance and comparison with the global synthesis of coeval coastal-onlap depositional sequences." @default.
- W2121998052 created "2016-06-24" @default.
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- W2121998052 date "1993-01-01" @default.
- W2121998052 modified "2023-09-23" @default.
- W2121998052 title "Eustatic and Tectonic Effects within Sequence Stratigraphy of the Outcropping Paralic-Marine Section, Upper Cretaceous, Alabama" @default.
- W2121998052 hasPublicationYear "1993" @default.
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