There is now strong evidence that stratal geometries on basin margins are most likely a
consequence of multiple controls, not just variations in accommodation. Consequently …

The sequence stratigraphic architecture includes a complex array of stratal geometries with
different degrees of stratigraphic significance. The 'non-unique'variability of the sequence …

Classic sequence stratigraphy suggests depositional sequences can form due to changes in
accommodation and due to changes in sediment supply. Accommodation‐dominated …

Confusions between methodology and modeling created a false premise to question the
'future of sequence stratigraphy'. In reality, the future is already here in terms of a standard …

The basic parameters that control stratal architecture in depositional sequences are
sediment flux, rate of change of sediment accommodation (ie, eustasy and sea-floor …

Stratal stacking patterns provide the key to the definition of all units and surfaces of
sequence stratigraphy, in a manner that is independent of the interpretation of the …

Sequence stratigraphy emphasizes facies relationships and stratal architecture within a
chronological framework. Despite its wide use, sequence stratigraphy has yet to be included …

Stratal stacking patterns provide the basis for the definition of all units and surfaces of
sequence stratigraphy. The same types of stacking patterns may be observed at different …

The interplay of local and global controls on accommodation and sedimentation generates
basin-specific sequence stratigraphic frameworks that record cyclicity at multiple scales …

Sequence stratigraphy emphasizes changes in stratal stacking patterns in response to
varying accommodation and sediment supply through time. Certain surfaces are designated …