Nadak Fm
Type Locality and Naming
Along the river Nadak, Kuramin Ridge. Z. P. Artemova in 1956 (411, p. 27). The stratotype is in the upper reaches of the Nadak River.
Synonym: Nadakskaya Suite, Надакская св.
Lithology and Thickness
At the base, there is a basal package (up to 350 m thickness) of conglomerates, sandstones, and siltstone (aleurolites) with rare layers of bituminous and siliceous limestones; above this, alternating conglomerates, sandstones, siltstone (aleurolites), tuffs, and ignimbrites of dacitic and andesidacitic composition, andesidacitic lavas, and less frequently andesites. The facies composition of the suite is characterized by extrusive domes. The thickness of the suite is 400-2500m.
Relationships and Distribution
Lower contact
Upper contact
Regional extent
Kuramin and Chatkal Suites in the Kuramin region within the Lashkerek, Adrasman, and Kyzylnurin volcano-structures and the eastern part of the Shavaz-Dukent graben.
GeoJSON
Fossils
In the lower part, plants that allow dating the age of the enclosing rocks to the Moscovian stage are found: Lepidodendron ex gr. worthenii Lesq., Neuropteris heterophylla Bron., Kandyria vasilkovskyi (Sixt.), Aulacotheca kandyrica Sav.; spores and pollen Leiotriletes inermis (Wal.), Lophotriletes verrucosus (Jbr.), Acanthotriletes hirtus Isch., Brachytrilistrium patullum Isch., Monoptycha (Ginkgo) cycadoformis Naum.; in the upper part, plants such as Sphenophyllum ex gr. majus (Bronn.), Sphenopteris marchalii Stock. et Math., Karabaupteris angrenica Sav., Gissarella kuramensis Sav., Cordaites schenkii Halle, Samaropsis czatkalensis Sav., Lebachia piniformis (Schloth.)
Age
Depositional setting
Additional Information