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ABSTRACT: Responses of a Deltaic System to Minor Relative Previous HitSeaNext Hit Previous HitLevelNext Hit Variations (Middle Jurassic, Cleveland Basin, England): Consequences on the Reservoir Geometry

R. Eschard, Ch. Ravenne, Heresim Group

In the Middle Jurassic series of the Cleveland basin (England), an accurate three-dimensional reconstruction of depositional Previous HitsequencesNext Hit from outcrops, cores, and wireline logs show that minor Previous HitseaNext Hit Previous HitlevelNext Hit variations control the evolution of a deltaic system. Because of low subsidence and sediment supply rates, rapid Previous HitseaNext Hit Previous HitlevelNext Hit rises induce several landward shifts of the shoreline, whereas minor Previous HitseaNext Hit Previous HitlevelNext Hit drops produce the incision of small paleovalleys.

The deltaic series, 200 m thick at the basin depocenter, are subdivided into five depositional Previous HitsequencesNext Hit. During the first two Previous HitsequencesNext Hit, the sediment supply rate exceeds the relative Previous HitseaNext Hit Previous HitlevelNext Hit rate and the delta progrades. The delta aggrades during the third depositional sequence and retrogrades in the fourth depositional sequence when the relative Previous HitseaNext Hit Previous HitlevelNext Hit rise rate balances then exceeds the sediment supply rate. Finally, a relative Previous HitseaNext Hit Previous HitlevelNext Hit drop induces the incision of a paleovalley progressively infilled during the following Previous HitseaNext Hit Previous HitlevelNext Hit rise.

Several orders of bathymetric Previous HitcyclesNext Hit are deduced from detailed correlations of the unconformities and from the comparison of the vertical facies succession between low and high subsiding areas. The general evolution of the delta is related to a 5-m.y. bathymetric cycle due to a eustatic Previous HitseaNext Hit Previous HitlevelNext Hit rise and fall. Pne to 3-m.y. bathymetric Previous HitcyclesNext Hit control the main aggradation patterns of the delta. These patterns are related to third-order eustatic Previous HitcyclesNext Hit or to local tectonic events. Less than 0.5 m.y. bathymetric Previous HitcyclesNext Hit are registrated by parasequences or minor depositional Previous HitsequencesNext Hit which are correlated all over the basin. The controlling parameters of the Previous HitsequencesNext Hit are discussed. Minor bathymetric Previous HitcyclesNext Hit (0.2 m.y.) reflect small-scale Previous HitseaNext Hit Previous HitlevelTop oscillations or autocyclic evolution of t e sedimentary bodies. We focus on the reservoir geometry within each bathymetric cycle.

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