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   Open Blocks: KSOUR ESSAF


 

GEOGRAPHICAL SETTING

Eastern offshore Tunisia.

ACREAGE

2108 km².

PREVIOUS EXPLORATION

About 2700 km of seismic have been shot and three wells have been drilled.

SEISMIC 

DATE

SURVEY

OPERATOR

SOURCE

NB OF Km

FIELD CONTRACTOR

1968

1985

1987

1992

1993

HG

SF85

SFf87

TWT92

RSS93

ELF/SEREPT

SANTA FE

SANTA FE

ETAP/CGG

BG

Vaporchoc

Airgun

Airgun

Airgun

Airgun

 500

800

700

200

500

CGG

GSI

Prakla

CGG

WESTERN

DRILLING

DATE

 WELL NAME

OPERATOR

TD (m)

 AGE at TD

SHOWS

1976

1979

1988

KSF-1

DEN-1

AM-1

ELF

TOTAL

SANTAFE

3135

2240

530

Aptian

Aptian

Aptian

Gas traces

Gas traces

Gas traces

GEOLOGICAL SETTING

The Ksour Essaf Block is part of a Mesozoic - Cenozoic platform with local highs characterized by dominated carbonate - shale deposits during the Jurassic to Mid-Miocene and siliciclastics deposits during the Mid-Late Neogene. The block includes two orthogonal highs:the SW-NE Kerkennah High Developed during Late Oligocene and remaind high to present time and the NW -SE Hana Ridge formed durind Turonian time.These pre-existent structures controlled over the block the sediment deposition and the facies distribution.

HYDROCARBON POTENTIAL

Reservoirs : The primary reservoirs are the Upper Senonian Abiod chalky limestones and Aptian Serdj carbonates. Secondary  targets include the Mid-Miocene Ain Grab and Oligocene Ketatna bioclastic limestones, Mid-Albian Allam limestones and Jurassic Nara dolomites. Most of these reservoirs tested oil and gas or gave oil and gas shows in the wells drilled within the block and  in the adjacent area.

Source Rocks : The Albian Fahdene shales and limestones provide the primary potential source in the area. Further potential is provided by the Mid-Cretaceous Aleg argillaceous limestones and Jurassic middle Nara black shales. The presence of  gas shows in Alfil#1 well and an oil column in the Halk El Menzel field, immediately west of the block, clearly indicates that source rocks are being mature.

Traps : They are dominated by fault blocks in addition to low amplitude anticlines initiated since the Mid-Cretaceous. Numerous prospects  are identified and awaiting to be drilled.