--> ABSTRACT: Dynamic Response of Carbonate Systems Tracts to Relative Sea Level Changes and the Development of Carbonate Depositional Sequences in Platforms and Ramps, by C. Robertson Handford, Robert G. Loucks; #91003 (1990).
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ABSTRACT: Dynamic Response of Carbonate Previous HitSystemsNext Hit Previous HitTractsNext Hit to Relative Previous HitSeaNext Hit Previous HitLevelNext Hit Changes and the Development of Carbonate Depositional Sequences in Platforms and Ramps

C. Robertson Handford, Robert G. Loucks

Some carbonate facies models are extremely useful for interpreting the paleoenvironments of most cratonic and shelf-margin carbonates, but these models do not address how environments and their depositional products respond to relative changes in Previous HitseaNext Hit Previous HitlevelNext Hit. Recently developed depositional sequence models, however, are answering those concerns. Although eustasy, tectonic subsidence, and sedimentation rates control relative Previous HitseaNext Hit Previous HitlevelNext Hit changes and are the most important factors controlling the development of carbonate depositional sequences, other important controls also need addressing: initial morphology (ramp or rimmed shelf), continental linkage (attached or detached), marine setting (oceanic vs. cratonic Previous HitseaNext Hit, open vs. closed seaway), latitude (tropical or temperate), mag itude of shelf (wide or narrow), climatic factors (orientation to wind and humidity), sediment type (carbonate, carbonate/clastic, carbonate/evaporite, and carbonate/evaporite/clastic), and age (Paleozoic with no calcareous pelagic oozes, post-Paleozoic with calcareous pelagic oozes). When combined with the widely acknowledged fact that siliciclastic and carbonate depositional principles are profoundly different, these factors mandate the need for developing a variety of carbonate depositional sequence models for rimmed shelves and ramps that demonstrate the autogenesis of carbonate sediments, the unique ability of carbonate environments to develop pronounced Previous HitseaNext Hit-floor topography, and the tendency of carbonate terrains to develop karst topography. Carbonate depositional sequence and syst ms tract models presented here are geologic based in that they were synthesized from modern and ancient carbonate Previous HitsystemsNext Hit. They represent idealized and expected responses to relative Previous HitseaNext Hit Previous HitlevelTop changes and assume total representation and preservation of products.

AAPG Search and Discovery Article #91003©1990 AAPG Annual Convention, San Francisco, California, June 3-6, 1990