Loralai Fm
Type Locality and Naming
Alozai Gr. – upper formation. Holotype section: Zamari Tangi. Author: Hunting Survey Corporation, 1960. Reference section: None.
Lithology and Thickness
Limestone. The formation consists mainly of well-bedded limestone with shale and marl interbeds in the lower part. The limestone is dark grey to black, weathers brownish grey, thin to thick bedded, hard, argillaceous, fine grained, and sub-lithographic and breaks with conchoidal fracture. Chert lenses are developed along the bedding planes. In the upper part, it contains oolitic, pisolitic and peletal beds at places. The shale is black, grey, splintery, peppery and calcareous. The marl is greenish grey and soft. The formation being resistant than the overlying Sembar Fm, forms prominent ridges in the area.
Thickness: 150-360 m. 250 m in the type section, 360 m in the Mara Tangi and 150 m in Tazi Ketch sections.
Relationships and Distribution
Lower contact
Conformably underlain by Spingwar Fm (transitional).
Upper contact
Disconformably overlain by Sembar Fm
Regional extent
The formation is widely exposed along a long strip in the northern Balochistan between Loralai and Zhob Valley (Axial Belt). [This seems to border or be in the Sulaiman Province = southern Indus Basin?]
GeoJSON
Fossils
Nejdia sp., Protogrammoceras sp., Phymatoceras sp. Rich in radiolarians.
Age
Depositional setting
Thin bedded, radiolarian and micritic limestone suggests low energy conditions.
Additional Information