Kuruk Fm
Type Locality and Naming
Named after the village of Kuruk, South Gissar. A.Ya. Frolenkova, Yu.S. Yurtaev, A.Kh. Chanyshev, 1966 (479, pp. 300–301). Stratotype near the village of Kuruk. The Kuruk Formation belongs to the Katkamysh Horizon (56; 446; 452).
Synonym: Kurukskaya Formation, Курукская св.
Lithology and Thickness
Composed of gray and dark-green clays and sandstones, and light-gray sandy limestones with rudists. Thickness 28–95 m.
Relationships and Distribution
Lower contact
Conformably overlies the Nilya Fm (South Gissar) or Gezan Fm (of Zarafshan district)
Upper contact
It is conformably overlain by the Akbulak-Cret Fm (South Gissar) or Khushikat Fm (of Zarafshan district).
Regional extent
South Gissar, Babatag Range, Zeravshan District.
GeoJSON
Fossils
Contains ammonites – Stantonoceras sp.; marine bivalves – Exogyra decussata Goldf., Megatrigonia syrdariensis (Arkh.), Anomia cryptostriata surkhandariensis Bobk.; foraminifers – Ammobaculites flabellamminaformis N. Byk., Gaudryinella pseudoasiatica N. Byk.
Age
Depositional setting
Additional Information