Kundalyantau Fm
Type Locality and Naming
By the ridge of Kundalyangtau, Southwest Gissar. Kh.Kh. Mirkamalov, 1971 (51, p.62). Stratotype in Kundalyangtau. Middle formation in Okuzbulak Gr. Corresponds to the middle (marine) part of the Okuzbulak Fm (Okuzbulak Gr) or the lower part of the Lower Okuzbulak Formation. S.N. Simakova. (55; 415; 452).
Synonym: Kundalyangtauskaya Suite, Кундалянтауская св.
Lithology and Thickness
At the bottom - gray and dark gray clays with layers of clayey limestones; at the top - alternation of siltstone (aleurolites), clays, greenish and brownish-gray limestones.
Relationships and Distribution
Lower contact
Lies conformably on the Machay Fm
Upper contact
It is conformably overlain by the Lyalimkan Fm
Regional extent
Southwest Gissar.
GeoJSON
Fossils
Contains ammonites Deshayesites ex gr. antiquas Bogd.; marine bivalve mollusks - Ceratostreon vinokurovae Mirk., Exogyra trigonalis Mirk.; foraminifera - Miliammina mjatliukae Dain., M. kuznetzovae S. Mam., Gyroidinoides sokolovae (Mjatl.); ostracods Antepraijenborchella praealta turkmenica Andrv., Asciocythere parabrevis Andrv. et Oertli. and a complex of spores and pollen.
Age
Depositional setting
Additional Information