Berkutlin Fm
Type Locality and Naming
Along the Berkutli River, northern slope of the Chumkartau Mountains, Turkestan Ridge. M.M. Posokhova, A.N. Golikov, 1973. (165, p.51). The stratotype is in the upper reaches of the Berkutli River.
Synonym: Berkutlinskaya Suite, Беркутлинская св., Berkyutlin Fm
Lithology and Thickness
In the Lower part, there are black and dark-gray sericitized argillaceous slates with lenses of siltstone (aleurolites), fthanite-like rocks, and phosphorites; in the Upper part - gray, greenish-gray sandy siltstone (aleurolites) with layers of sericitized slates and coalified argillites. Thickness in different regions from 60 to 200-300 m.
Relationships and Distribution
Lower contact
Conformably lies on the Guralash Fm
Upper contact
Conformably covered by the Uryuklin Fm.
Regional extent
Chumkartau Mountains.
GeoJSON
Fossils
Contains graptolites - Cephalograptus tubulariformis (Nich.), C. cometa (Gein.), Monograptus sedgwicki (Portl.), Demirastrites convolutus (His.), Rastrites peregrinus Barr. and others, Middle Llandovery.
Age
Depositional setting
Additional Information