It is important
to understand that depositional environments are not randomly
distributed across the platform interior, 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 as to the
control of relative sea-level changes on the placement of the
different depositional environments. The reader can refer to Handford
and Loucks (1993) for a basic discussion on relative sea-level
changes on carbonate system tracts.
Review
the general discussion on processes that is presented in the pop
up menu below. As you study each major depositional environment,
be sure to think of each of these processes and how each of these
processes affects the creation and deposition of carbonate sediments.
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