Data Package Contents

Dr. Michael GardoshHead 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

2D seismic surveysTGS 2001 survey (64 lines) SEGY

TGS 2008 survey (19 lines) SEGY

GravitySurvey line data, grids and processing report (TGS 2001

survey)ASCII

MagneticSurvey line data, grid and processing report (TGS 2001

survey)ASCII, PDF

Bathymetry Grid and technical report ASCII, PDF

Regional reports

Highlights of Basin Analysis of the Levantine Basin Offshore -

extracted from the BeicipFranLab Final Report (2015)PDF

The Levant Basin Offshore Israel: Stratigraphy, Structure,

Tectonic Evolution and Implications for Hydrocarbon

Exploration. Revised Addition – Gardosh et al., (2008)

PDF

Data Package-Well Locations

Mediterranean Sea

Mediterranean Sea

Data Package-Summary of Well Information

Mediterranean Sea

Offshore Israel

wells

LAS

files

Reports

Velocity

SurveyEOWR

Composite

Log

Reservoir

Characterization

EOWR

Formation

Evaluation

Stratigraphy/

PaleontologyGeochemistry

1

ANDROMEDA EAST

01 V V V V V

2

APHRODITE 02

(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

12

OR SOUTH

01/01A/01B V V V

13 QISHON YAM 01 V V V V V

14 SARA 01 V V V V V V

15

YAM 01

(+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)

Aphrodite 02TWT

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

The Neo-Tethyan tectonic activity initiated the development ofthe stretched Levant margin in the early Jurassic time.

At the end of the Cretaceous, a regional transpressive eventtriggered the inversion of extensional structures in the easternpart of the basin leading to the development of the present-daymargin configuration.

The subsidence history graphs (on the left) illustrate the evolutionof two structural domains. The graphs show that the tectonicsubsidence shows a typical lithospheric thermal decay since theJurassic in the deep offshore. For the Upper Slope, the tectonicsubsidence halts during the Paleogene-Neogene as a consequenceof the tectonic compression. The total subsidence results fromchanging sedimentation rates in a gently subsidizing basin.

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 to10-12km in the central part of the basin is generally well definedby seismic refraction and gravity models. (Ben-Avraham et al.,2002)

The thin crust in the central Levant is most likely an extendedand attenuated continental crust that is associated with lowerheat-flow when compared to the heat-flow of the eastern shelfand margin/slope.

Adapted from Ben-Avraham et al (2002)

Deep offshore Upper slope

1 km

1 km

Highlights of Basin Analysis (BeicipFranLab Report)

Additional Data - 3D Seismic Coverage

Mediterranean Sea

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