This post about lapouts (onlap, toplap, downlap, offlap, truncation) is a companion to Clinoforms and
Category: Interpreting ancient environments
Earth’s surface is a time plane. It is a plane of deposition and erosion, of chemical
Stratigraphic trends in outcrop and core, and the role they play in identifying parasequence stacking
A brief look at identifying shoreline trajectories in stratigraphic successions. This post is part of
Parasequences are the building blocks of shallow marine systems tracts. The stratigraphy of ancient,
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