Kofrun-Cret Fm
Type Locality and Naming
Along the village of Kofrun, South-West Gissar. Kh.Kh. Mirkamalov, M.E. Egamberdyev, 1969 (300, p.62). Stratotype in 15-20 km to the southeast of the village of Kofrun. Uppermost formation in Tally-Khumon Gr
Synonym: Kofrun Suite, Кофрунская св.
Lithology and Thickness
In the south - brecciated limestones, sandstones, marls with gypsum interlayers in the lower part (thickness 8-50m); in the north - gray siltstone (aleurolites), limestones, sandstones with interlayers of red-colored clays (thickness 5-20m).
Relationships and Distribution
Lower contact
Conformably overlies the Udan-Tau Fm
Upper contact
It is overlain with erosion by the Bukhara Fm of the Paleocene.
Regional extent
GeoJSON
Fossils
Contains marine bivalve mollusks - Liostrea lehmannii Rom., Chlamys dujardini Roem.; foraminifers - Orbitoides media Arch.
Age
Depositional setting
Additional Information