--> Abstract: Recent Advances in Sequence Stratigraphy: The Lowstand and Transgressive Systems Tracts, by H. W. Posamentier and G. P. Allen; #90990 (1993).
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POSAMENTIER, HENRY W., ARCO Exploration and Production Technology, Plano, TX; and GEORGE P. ALLEN, TOTAL Centre Scientifique et Technique, St. Remy les Chevreuses, France

ABSTRACT: Recent Advances in Sequence Stratigraphy: The Lowstand and Transgressive Previous HitSystemsNext Hit Previous HitTractsNext Hit

On basin margins characterized by a ramp physiography, relative Previous HitseaNext Hit Previous HitlevelNext Hit fall induces basinally isolated, shelf-perched, forced-regression shoreline and deltaic deposition rather than deep-water submarine-fan turbidite deposition. These deposits comprise the early lowstand Previous HitsystemsNext Hit tract. In proximal locations, the sequence boundary at the base of these lowstand deposits is expressed as an erosional unconformity, whereas in distal settings this surface occurs as a correlative conformity. The stratigraphic discontinuity at the top of these lowstand deposits is a ravinement surface and in places can be more striking than the sequence-bounding surface at the base. Significant erosion due to fluvial processes during forced regression and subsequent shoreface processes during transgression may be common at the tops of these lowstand deposits.

The transgressive Previous HitsystemsNext Hit tract commonly comprises, proximally to distally, backstepped barrier beach deposits, sheet-like lag deposits, and "healing Previous HitphaseNext Hit" deposits. This latter unit has not been described widely, but volumetrically may contain a significant part of the transgressive Previous HitsystemsNext Hit tract. Healing Previous HitphaseNext Hit deposits comprise a wedge of sediment that onlaps the last clinoform of the underlying progradational Previous HitphaseNext Hit. These sediments commonly are derived by cannibalization from the top or edge of the subjacent progradational Previous HitphaseNext Hit deposits (i.e., either highstand or lowstand), during and immediately after transgression. These deposits are referred to as the healing Previous HitphaseNext Hit because their deposition tends to "heal over" the relatively steep clinoform slope of the underlying progradation l Previous HitphaseTop after transgression has resulted in landward shift of the depocenter. Although sometimes misinterpreted as lowstand deposits, these depositional units commonly do not contain significant reservoir facies.

AAPG Search and Discovery Article #90990©1993 AAPG International Conference and Exhibition, The Hague, Netherlands, October 17-20, 1993.