Turkestan Horizon Gr
Type Locality and Naming
Along the Turkestan suite, Fergana. A.A. Abdusamatov et al., 1988. Unites Alay Fm, Syrenyatin Fm, Turkestan Fm, Rishkan Fm, Malanddarin Fm.
Synonym: Turkestan Horizon, Туркестанский гор.
Reference section:
Lithology and Thickness
Gray, light-gray sandstones, limestones; green, tobacco-green clays. Thickness 380m.
Relationships and Distribution
Lower contact
Conformably overlies the Suzak horizon
Upper contact
Conformably overlain by the Kushan horizon
Regional extent
Fergana Depression, South of Gissar, Prishchekent District. Correlated with the Kuberdin and Kum Mountains of South Uzbekistan.
GeoJSON
Fossils
Characterized by a complex of marine bivalve mollusks - Ostrea turkestanensis Rom., O. pseudobellovacina Kachan., Lucina consobrina Desh., Pitar gumberensis Arch., Cardium porulosum Sol., Tellina ziddiensis Kachan. and others; foraminifera - Bermudesina pseudonavarroana (Balakhm.), Discorbis ferganensis N. Byk., Acarinina bullbrooki Bolli. in the lower part; marine bivalve mollusks - Pleurodon baskarensis Korob. et Makar., Chlamys vialovi Korob., Fatina böhmi Vial., Liostrea kokanensis Sok., Lucina menardi Desh., Cardium porulosum Desh., Pitar laevigata Lam., Panope oppenheimi Korob. and others; foraminifera Discorbis ferganensis N. Byk., Eponides Jacksonensis Cushm., Acarinina rotundimarginata Subb., Uvigerina costellata Moroz. in the middle part and marine bivalve mollusks - Ostrea simplex Desh., Platigena asiatica Rom., Pitar gumberensis Arch. and others; foraminifera - Popovia rugosa Sul., Gaudryina superturkestanica N. Byk., Discorbis ferganensis N. Byk., Asianella vialovi N. Byk., Caucasinella pseudoelongata (N. Byk.) in the upper part.
Age
Depositional setting
Additional Information