Almurad Fm
Type Locality and Naming
Along Almurad Mountain, South-Western Gissar. N.P. Kheraskov, 1934 (487, p.18). In the Bukhara-Karshinsky region, well exposed. Stratotype at r. Almurad. Middle formation in the Takchiyan Gr. Included in the Almurad horizon (55; 115; 133; 167; 274; 362; 415; 445; 498).
Synonym: Almurad Suite, Алмурадская св.
Lithology and Thickness
The formation is predominantly three-membered in structure.
At the bottom - clays, siltstone (aleurolites), reddish-brown sandstones with gypsum interlayers;
Middle part - marls, dolomites, bluish-gray clays, in the north (Lyangar, Chakchar, Machay) - reddish-brown clays, siltstone (aleurolites), gypsums with interlayers of gray sandstones and gravelites;
At the top - siltstone (aleurolites), reddish-brown clays with gypsum interlayers.
In the Babatag Ridge, the formation is composed of reddish-brown clays with gypsum interlayers.
Thickness 36-195m.
Relationships and Distribution
Lower contact
Lies conformably, locally transgressively on the Karabil Fm
Upper contact
Conformably overlain by the Kyzyltash Fm.
Regional extent
Southwestern, Southern Gissar, Babatag Ridge.
GeoJSON
Fossils
Contains marine bivalve mollusks - Lima tombeckiana Orb., Pterotrigonia caudata (Ag.), Astarte beamonti Orb.; ostracods - Malzevia ex gr. pellucida (And.).
Age
Depositional setting
Additional Information