Parasequences are the building blocks of shallow marine systems tracts. The stratigraphy of ancient,
Category: Interpreting ancient environments
A brief look at the key stratigraphic surfaces that help us construct sequence stratigraphic models.
Stratigraphic repetition, stratigraphic cycles, and stratigraphic trends We know with reasonable certainty that the sun
Or why the distinction between allogenic and autogenic dynamics is not as straight forward as
One of the beaches we frequent, off the beaten track and commonly deserted, has at
Changes in sea level, or baselevel, are central to all forms of genetic stratigraphy. Shorelines
Facies and facies models are fundamental tools for sedimentology and sequence stratigraphy. This is part
The duality of stratigraphic accommodation and sediment supply This is part of the How To…series
Baselevel is a datum. This is part of the How To…series on Stratigraphy and Sequence
This is the third of three posts that look briefly at the development of stratigraphic