Saratash Fm
Type Locality and Naming
Includes in SE Murghab district (Istyk type Dunkeldyk area). It is distinguished by V. I. Dronov in 1968.
Synonym: Sarytash Fm, Saratashskaya suite, сарыташская свита
Reference section:
Lithology and Thickness
It is universally divided into three parts. The lower part of the suite (Djangisuy member (джангисуйская Толща)), with a thickness of up to 45 m, is composed of finely layered cherts with limestone interlayers; the middle (Bosterek member (бозтеринская толща), with a thickness of up to 15 m, is composed of massive and coarse-bedded limestones; the upper (Kurudzhilgin member), with a thickness of up to 25 m, is composed of finely layered cherts and calcareous-chert shales with limestone interlayers.
Relationships and Distribution
Lower contact
Upper contact
It is overlain conformably by the Istyk Fm of Norian-Rhaetian.
Regional extent
It is widespread in the Southeast Pamir.
GeoJSON
Fossils
Organic remains are contained in all members. The Djangisuy member at the bottom includes Anisian-Ladinian pelecypods - Posidonia wengensis W.issm., P. alta Mojs. et al., in the middle and upper parts - Ladino-Carnian pectinids - Daonella pichleri Bitt., D. reticulata Mojs., D. indica Bitt. The Bozterinskaya formation contains Early Carnian ammonoids - Jovites aff. daci Mojs., Tropites estellae Mojs. Kyruzhilgin member contains abundant remains of Late Carnian-Early Norian pectinids Halobia austriaca Mois., H. cassiana Mojs., H. charlyana Mojs.
Age
Depositional setting
Additional Information