Shoreline and shelf‐edge trajectories describe the migration through time of sedimentary
systems, using geomorphological breaks‐in‐slope that are associated with key changes in …

Shoreline migration patterns can be described in terms of the shoreline trajectory, which is
the shoreline path viewed along a cross-sectional depositional-dip section. Discrete classes …

Abstract Sequence stratigraphic models are:(1) discussed from a theoretical point of view,
with emphasis on a systematical discussion of the breakdown of depositional cycles …

The sequence‐stratigraphic signature of a shoreline excursion is controlled by sediment
accumulation rates relative to the distribution and rates of generation of accommodation …

The future of sequence stratigraphy depends on stratigraphers making observations with a
common method so that physical frameworks can be clearly separated from interpretations …

ABSTRACT The Shelf Edge and Shoreline Trajectories Conference, convened in Tromsø,
Norway, during the autumn of 2007, was attended by a group of specialists working in the …

We propose a framework for the hierarchy of sedimentary units observed in stratigraphic
data that is based entirely on the geometric relationship of the strata. This framework of …

Sequence stratigraphic concepts suggest that stratal geometries develop and are largely
controlled by changes in relative sea level. On the shelf, lowstand deposits, which form …

The recurrence of the same types of sequence stratigraphic surface through geologic time
defines cycles of change in accommodation or sediment supply, which correspond to …

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