Shiberdzhilgin Fm
Type Locality and Naming
Includes in East Pshart, East Pshart (southern slope), East Pshart (Agadjan river basin). It is identified in 1968 by V.I. Dranov.
Synonym: Shiberdzhilginskaya formation, шиберджилгинская толща
Reference section:
Lithology and Thickness
70 m thick, is composed of greenish, sometimes dirty-red tuffs and tuff conglomerates of basic rocks with interlayers of colorful cherts and nodules, fragments of white organic limestones
Relationships and Distribution
Lower contact
Upper contact
overlain with unclear relationships by dark gray sandstones and slates, which are conditionally attributed to the lower - middle Triassic.
Regional extent
They outcrop in the watershed and on the northern slope of the eastern part of the Shart Range.
GeoJSON
Fossils
It consists of foraminifera Codonofusiella sp., Rauserella sp., Kahlerina sp., Misellina sp., etc.
Age
Depositional setting
Additional Information