Tigi Formation

Tigi Fm

Period:

Jurassic

Age Interval:

Aalenian – Callovian.

Province:
Oued Mya Basin, Ghadames Basin

Type Locality and Naming

Synonym:

References: Klett, 2000.

Lithology and Thickness

The Tigi Fm is characterized by Mudstone, sandstone, limestone, and basal anhydrite; diagrammed as mainly clayey limestone (Klett, 2000).

Lithology Pattern:

Clayey limestone

Relationships and Distribution

Lower contact

It conformably overlies the Saliferous Units Fm.

Upper contact

It is conformably overlain by the Shakshuk Fm.

Regional extent

GeoJSON

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Fossils

Age

Middle Jurassic (Klett, 2000, diagram)

Age Span:

Beginning stage:

Aalenian

Fraction up in beginning stage:

0.00

Beginning date (Ma):

174.70

Ending stage:

Callovian

Fraction up in the ending stage:

1.0

Ending date (Ma):

161.53

Depositional setting

Depositional pattern:

Additional Information

Compiler:

Enam O. Obiosio, Solomon Joshua Avong and Henry Nasir Suleiman (2024) - Stratigraphic Lexicon compiled from the following books:

Baouche, R., Ganguli, S. S., Sen, S., Radwan A. E. (2023): Assessment of reservoir stress state and its implications for Paleozoic tight oil reservoir development in the Oued Mya Basin, northeastern Algerian Sahara. Geosystems and Geoenvironment 2: pp.1-18. https://doi.org/10.1016/j.geogeo.2022.100112

Fadila B. (2004): Reservoir Characterization and Reservoir Modeling in the Northwestern Part of Hassi Massaoud Field Algeria. A PhD thesis at the University of Hamburg, Hamburg, Germany.

T.R. Klett (2000): Total Petroleum Systems of the Trias/Ghadames Province, Algeria, Tunisia, and Libya - The Tanezzuft-Oued Mya, Tanezzuft-Melrhir, and Tanezzuft-Ghadames. U.S. Geological Survey Bulletin, 2202-C.

Kraouia et al., (2023): Ordovician–Upper Silurian–Triassic Petroleum System Assessment in the Chotts Area. In S. Khomsi and F. Roure (eds.), Geology of North Africa and the Mediterranean: Sedimentary Basins and Georesources, Regional Geology Reviews, https://doi.org/10.1007/978-3-031-18747-6_7