[First Hit]

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Rob L. Gawthorpe1, Ian Sharp2, Christopher A. Jackson1, Mike Young1

(1) University of Manchester, Manchester, United Kingdom
(2) Norsk Hydro Research Center ASA, Bergen, Norway

ABSTRACT: Integrated Structural and Sequence Stratigraphic Analysis Reveals the Spatial and Temporal Evolution of Normal Previous HitFaultNext Hit Arrays; Suez Rift, Egypt

Pseudo-3D exposure of Miocene syn-rift sequences and normal Previous HitfaultNext Hit zones from the Suez rift provide exceptional outcrop analogues for structural styles and stratigraphic responses in evolving normal Previous HitfaultNext Hit populations. Surface deformation associated with growth and linkage of Previous HitfaultNext Hit segments is reflected by characteristic changes in the three-dimensional form of depositional sequences, their internal stratal geometry and bounding stratal terminations. Here we use these parameters, within key stratigraphic intervals, to reconstruct the early stages of Previous HitfaultNext Hit array evolution from the southern portion of the Hammam Faraun Previous HitfaultNext Hit block. The present-day structural style of this area comprises a 10-15 km wide half graben bounded by 25-50 km long Previous HitfaultNext Hit zones with kilometres of displacement. Results indicate that the early syn-rift structural style was markedly different to that suggested by the present-day structural geometry.

Early stages in the evolution are characterised by numerous, small isolated depocentres. These depocentres were typically <4 km long and 1-2 km wide, reflecting the size of the early normal Previous HitfaultNext Hit segments. Stratal geometries and thickness distributions indicate that many of these early depocentres were controlled by growth folds above blind normal faults. Within the first few million years of rifting, some of these faults propagated upward to break surface, and linked to form Previous HitfaultNext Hit zones up to 10 km long. During this time interval, other Previous HitfaultNext Hit zones died and were overstepped by syn-rift deposits. Deformation did not localise onto the major half graben bounding Previous HitfaultTop zones until some 5-7 million years after the onset of rifting.

AAPG Search and Discovery Article #90906©2001 AAPG Annual Convention, Denver, Colorado