Donguztau Fm
Type Locality and Naming
Along the Donquztau elevation, Central Kyzylkum. I.M. Abdurazimova, 1988 (24, p.65). The stratotype is located on the southwestern slope of the Kuljuktau mountain, 24 km southeast of the Donquztau elevation, along the Jamanjar (Dzhamanyar) say.
Synonym: Donguztau Suite, Донгузтауская св.
Lithology and Thickness
Coastal-marine, interbedded with continental, greenish-gray, yellow, variegated gravels, sandstones, siltstone (aleurolites), clays with interbeds of conglomerates. Thickness 11-120m.
Relationships and Distribution
Lower contact
Along the bedding, it lies with erosion on the Shuruk-Cret Fm and transgressively on the Paleozoic. In the schematic stratigraphic column of Takhatau, it lies with erosion on the Bassay Fm. In Tamdytau, with Kynyr-Perm Fm
Upper contact
It is overlain with erosion by the Uchkuduk-Cret Fm.
Regional extent
Central Kyzylkum, foothills of Kuljuktau, Auminzatau, Tamdytau, Nurata Mountains; exposed in plains by wells. It is correlated with the Tyubegatan Fm, Karikansay Fm, and Tagarin Fm of the South Gissar.
GeoJSON
Fossils
Contains marine bivalve mollusks Exogyra trigeri Coq., Lopha dichotoma Bayle.; foraminifera - Trochamminoides cenomanicus (Zhuk.); dinosaur bone fragments and wood; spores and pollen.
Age
Depositional setting
Coastal-marine
Additional Information