Rangkul Fm
Type Locality and Naming
Includes in Akbaital-Rangkul region. It was identified in 1937 by P.D. Vinogradov.
Synonym:
Reference section:
Lithology and Thickness
It is composed of massive and coarsely bedded reef limestones up to 500-800 m thick, lying in a tectonic schist.
Relationships and Distribution
Lower contact
Upper contact
Regional extent
It is widespread in the Central Pamir, in the zone of the southern Rangkul tectonic schists.
GeoJSON
Fossils
Organic remains have mostly been collected in debris and are not strictly tied to the section. Among them, Early Triassic-Anisian pelecypods Myophoria cf. laevigata Zieth., Eumorphotis cf. venetiana (Hauer); Anisian ammonoids Monophyl] lites cf. sphaerophyllus (Hauer), Leiophyllites aff. pitamaha Dien.; brachiopods Tetractinella cf. trigonella Schloth., Spiriferina cf. fragilis Schloth.; Ladinian-Carnian and Carnian pelecypods Aviculopecten cf. wissmani Münst., Lima cf. subpunctata Orb., Amonotis sp.
Age
Depositional setting
Additional Information