It
is important to understand that depositional environments
are not randomly distributed across the platform, slope,
or basin but form in response to well-organized physical, biological,
and chemical processes. Therefore, predictable patterns of depositional
environments develop. The generalized platform model is simplified
regarding control of relative sea-level changes on the placement
of different depositional environments. The reader can refer to
Handford and Loucks (1993) for a basic discussion about relative
sea-level changes on carbonate systems tracts.
Review the
general discussion on processes that is presented next under the
pop-up menu. As you study each major depositional environment,
be sure to think about each of these processes and how each affects
the creation and deposition of carbonate sediments. |