--> Evolution of Normal Faults: Displacement Patterns in 3-D Seismic From the Eastern Levant Basin
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AAPG Geoscience Technology Workshop

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Evolution of Normal Faults: Displacement Patterns in 3-D Seismic From the Eastern Levant Basin

Abstract

The continental shelf offshore Israel is densely populated by slump units in the Pliocene -Pleistocene section. The gigantic unit known as the Israel Slump Complex (ISC) and its overburden are incised by thin-skinned Previous HitfaultNext Hit systems. Quantitative Previous HitfaultNext Hit displacement analysis presents the relation between the slump units and the evolution of normal faults incising them. Following structural standard Previous HitinterpretationNext Hit, slump units and an array of normal faults and are mapped in the Gabriella seismic volume, a high-resolution 3D seismic survey (depth-migrated) located 12 km offshore Netanya. The Previous HitstratigraphicNext Hit column of the volume includes the post-Messinian section of Saqiye and Kurkar groups. Previous HitFaultNext Hit systems are characterized by unrestricted blind faults and restricted growth faults. The Middle-Late Pleistocene progradational settings make distinguishing the two types of faults a challenge. Previous HitFaultNext Hit displacements are analyzed based on ten key horizons using a step-by-step workflow which includes throw-versus-depth profiles, displacement contour diagrams and displacement gradients. Growth stages within the faults are highlighted using expansion indices and restoration models. Combination of these methods proves useful both for growth model classification and accurate Previous HitfaultNext Hit mapping. Variations in displacement patterns underscore the control of chaotic features, acting to restrict the growing faults. Two main Previous HitfaultNext Hit zones are identified: Northern Previous HitFaultNext Hit Zone (NFZ) and Southern Previous HitFaultNext Hit Zone (SFZ), comprised of N-S and NW-SE striking normal faults, respectively. Four sampled faults yield distinguishable types of growth: (1) Blind Previous HitfaultNext Hit, where both horizontal and vertical tips close gradually; (2) Restricted growth Previous HitfaultNext Hit initially evolving as a blind Previous HitfaultNext Hit, associated with an incision into the ISC at 0.51-0.7Ma; (3) Blind Restricted Previous HitfaultNext Hit, with two zones of high displacements, associated with the incision of a small slump unit; (4) Blind restricted Previous HitfaultNext Hit, characterized by high displacement gradients at its deeper part. Maximum displacement zones imply the faults nucleated at 600-700m depth. The restricted growth Previous HitfaultNext Hit is characterized by shallower maximum displacement zone, interpreted to result from a transition from blind to growth propagation. We find that chaotic structures control Previous HitfaultNext Hit activation, which depends on the spatial relation between the structures. This can result either locally with segmented activation within the Previous HitfaultNext Hit, or with lateral growth initiation on the entire Previous HitfaultNext Hit. The linkage between proximity to slump units and growth pattern may lie in the compaction potential of the latter. The research provides empirical evidence for distinguishing a Previous HitfaultNext Hit growth and blind stages. This can be especially helpful where faults have similar dimensions and ranges of throw values, which result in minor displacement differences. The presented workflow can also be used for illuminating geo-hazards related to Previous HitfaultTop activation.