--> Fluid Flow Systems Within the Plio- Quaternary Succession in the Levant Basin, Offshore Central Israel
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Previous HitFluidNext Hit Previous HitFlowNext Hit Systems Within the Plio- Quaternary Succession in the Levant Basin, Offshore Central Israel

Abstract

The present study focuses on investigating seismo-geomorphologic manifestations of Previous HitfluidNext Hit Previous HitflowNext Hit in the Plio-Quaternary deposits, overburdening the offshore hydrocarbon province within the Levant Basin, SE Mediterranean Sea. We present the analysis of a new three-dimensional (3D) high-resolution seismic data, spanning ∼1440 sq km in water depths ranging 1100m to 1500m offshore central Israel. Controls for our study are petrophysical logs from two deepwater wells. Seismic stratigraphic techniques and robust seismic attribute workflow has promoted the recognition of evidences for Previous HitfluidNext Hit Previous HitflowNext Hit in the study area expressed as acoustic anomalies observed in the 3D seismic data. Preliminary results reveal at high resolution Previous HitfluidNext Hit Previous HitflowNext Hit structures encompassing dissolution pipes, pockforms and zones of chaotic reflections within the Plio-Quaternary succession, all emanating from the top Messinian evaporite unit. These features are spatially grouped into two populations, with the western part of the study area predominating with Previous HitfluidNext Hit Previous HitflowNext Hit structures compared to the eastern. The lack of evidences for focused Previous HitfluidNext Hit Previous HitflowNext Hit beyond the successive mass transport deposits emplaced and the seafloor, with the exception of enhanced reflectivity in paleo-channels, suggest a casual mechanism between decimation of possible Previous HitfluidNext Hit Previous HitflowNext Hit features and mass wasting events during the Plio-Quaternary. We invoke the origin of the Previous HitfluidNext Hit Previous HitflowNext Hit systems to be related to evaporite–Previous HitfluidNext Hit interaction in the Messinian evaporite substratum and subsequent Previous HitfluidNext Hit transport through migration pathways into the Plio-Quaternary unit. Understanding the Previous HitfluidNext Hit Previous HitflowNext Hit systems exemplified here has important implications for geohazards risk assessment, contributes to our understanding of Previous HitfluidNext Hit Previous HitflowTop subsequent to the Messinian salinity crisis and as an analog to other sedimentary basins and margins.