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ABSTRACT: Computer Models for Defining Eustatic Previous HitSeaNext Hit Previous HitLevelNext Hit Fluctuations in Previous HitCarbonateNext Hit Rocks

J. F. Read, M. E. Elrick, D. A. Osleger

One- and two-dimensional computer models of Previous HitcarbonateNext Hit Previous HitsequencesNext Hit help define the amplitudes and periods of 20,000 years to 1 m.y. and 1-3 m.y. Previous HitseaNext Hit Previous HitlevelNext Hit fluctuations that have affected Previous HitcarbonateNext Hit rocks. The models show that with low-amplitude 20-100 k.y. Previous HitseaNext Hit Previous HitlevelNext Hit fluctuations, tidal flats are likely to extend across the platform during short-term regressions, and vadose diagenesis is limited because Previous HitseaNext Hit Previous HitlevelNext Hit rarely drops far below the platform surface. With high-amplitude 20-100 k.y. Previous HitseaNext Hit Previous HitlevelNext Hit fluctuations, tidal flats are confined to coastal locations, very deep-water facies are overlain by shallow-water beds, and during regression Previous HitseaNext Hit Previous HitlevelNext Hit falls far below the platform, leaving karstic surfaces. The models also allow testing of random vs. Milankovitch-driven Previous HitseaNext Hit Previous HitlevelNext Hit c anges. The feasibility of cyclic sedimentation due to autocyclic processes under static Previous HitseaNext Hit Previous HitlevelNext Hit can be shown by the modeling to be less likely than Milankovitch climatic forcing for developing cyclic Previous HitcarbonateNext Hit Previous HitsequencesNext Hit. Models also help define relative dominance of 100 k.y. vs. 20 or 40 k.y. Previous HitseaNext Hit Previous HitlevelNext Hit oscillations. The presence of shallow-ramp vs. deep-ramp upward-shallowing Previous HitcyclesNext Hit that are common on many platforms provides valuable constraints on the modeling in that the Previous HitseaNext Hit Previous HitlevelNext Hit fluctuations generating the shallow Previous HitcyclesNext Hit also have to be able to generate the deeper ramp Previous HitcyclesNext Hit. Previous HitSeaNext Hit Previous HitlevelNext Hit fluctuations of 1-3 m.y. are constrained by the modeling because overestimated amplitudes result in Previous HitsequencesNext Hit and high-frequency Previous HitcyclesNext Hit that are far too thick. Rate of long-term falls are constraine by the modeling because where fall rate exceeds driving subsidence, the outer platform becomes unconformable, whereas it remains conformable where fall rate is below driving subsidence rate. Quantitative modeling techniques thus provide the means of constraining amplitudes and frequencies of eustatic Previous HitseaNext Hit Previous HitlevelNext Hit fluctuations in ancient Previous HitcarbonateNext Hit Previous HitsequencesTop.

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