Data Package Contents Dr. Michael Gardosh Head of Geology and Geophysics Department Ministry of National Infrastructure, Energy and Water Resources
Data Package Contents Data type Data content Format Well data and reports 20 deep wells LAS, PDF TGS 2001 survey (64 lines) SEGY 2D seismic surveys TGS 2008 survey (19 lines) SEGY Survey line data, grids and processing report (TGS 2001 Gravity ASCII survey) Survey line data, grid and processing report (TGS 2001 Magnetic ASCII, PDF survey) Bathymetry Grid and technical report ASCII, PDF Highlights of Basin Analysis of the Levantine Basin Offshore - PDF extracted from the BeicipFranLab Final Report (2015) Regional reports The Levant Basin Offshore Israel: Stratigraphy, Structure, Tectonic Evolution and Implications for Hydrocarbon PDF Exploration. Revised Addition – Gardosh et al., (2008)
Data Package-Well Locations Mediterranean Sea Mediterranean Sea
Data Package-Summary of Well Information Reports Offshore Israel LAS wells files Reservoir Velocity Composite Formation Stratigraphy/ EOWR Characterization Geochemistry Survey Log Evaluation Paleontology EOWR ANDROMEDA EAST 1 01 V V V V V APHRODITE 02 2 (ISHAI) V V V V 3 ASHER YAM 01 V V V V V 4 BRAVO 01 V V V V V 5 DELTA 01 & 01A V V V V 6 FOXTROT 01 V V V V 7 GAD 01 V V V V V 8 HANNAH 01 V V V V V 9 MYRA 01 V V V V V V V 10 NIR 01 V V V V 11 OR 01 V V V OR SOUTH Mediterranean Sea 12 01/01A/01B V V V 13 QISHON YAM 01 V V V V V 14 SARA 01 V V V V V V YAM 01 15 (+SIDETRACK) V V V V 16 YAM 02 V V V V V V 17 YAM 03 V V V V V 18 YAM WEST 01 V V V V 19 YAM WEST 02/02A V V V V 20 YAM YAFO 01 V V V V
Data Package-Example of Wirline Log Plots
Data Package-Examples of Well Reports
Data Package- Location of 2D Seismic Lines Mediterranean Sea
Data Package – Example of 2D Seismic Profile (TGS 2001) TWT Hannah 01
Data Package – Example of 2D Seismic Profile (TGS 2008) TWT Aphrodite 02
Data Package – Example of 2D Seismic Profile (TGS 2001) TWT Myra 01
Data Package-Gravity and Magnetic Coverage Mediterranean Sea
Data Package-Gravity and Magnetic Grids
Highlights of Basin Analysis (BeicipFranLab Report) CRUSTAL STRUCTURE AND SUBSIDENCE HISTORIES OF THE LEVANT BASIN The crustal nature of the Levant basin is still a matter of debate, but thick continental crust (30-35 km) in the east that thins to 10-12km in the central part of the basin is generally well defined by seismic refraction and gravity models. (Ben-Avraham et al., 2002) The thin crust in the central Levant is most likely an extended and attenuated continental crust that is associated with lower heat-flow when compared to the heat-flow of the eastern shelf and margin/slope. Adapted from Ben-Avraham et al (2002) The Neo-Tethyan tectonic activity initiated the development of the stretched Levant margin in the early Jurassic time. Deep offshore Upper slope At the end of the Cretaceous, a regional transpressive event triggered the inversion of extensional structures in the eastern part of the basin leading to the development of the present-day 1 km margin configuration. The subsidence history graphs (on the left) illustrate the evolution 1 km of two structural domains. The graphs show that the tectonic subsidence shows a typical lithospheric thermal decay since the Jurassic in the deep offshore. For the Upper Slope, the tectonic subsidence halts during the Paleogene-Neogene as a consequence of the tectonic compression. The total subsidence results from changing sedimentation rates in a gently subsidizing basin.
Additional Data - 3D Seismic Coverage Mediterranean Sea
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