Chashmaobzan Fm
Type Locality and Naming
Along the ridge of outcrops, located south of the Tashkent-Termiz highway, S.W. Gissar. Kh.Kh.Mirkamalov, M.E.Egamberdyev, 1969 (300, p.64). Stratotype - ridge of outcrops, located south of the Tashkent-Termiz highway, between the meridians of the Kana River and the Akbrat settlement. Lower formation in Adamtash Gr
Synonym: Chashmaobzan Suite, Чашмобазинская св., Talhab Fm (446).
Lithology and Thickness
Upper part - clays with layers of siltstone (aleurolites).
Lower part - greenish-gray clays with light marls and calcareous siltstone (aleurolites), at the base of the suite
Total thickness 100-200m.
Relationships and Distribution
Lower contact
Conformably overlies the Gazdagan Fm
Upper contact
It is also overlain by the Dekhkanabad Fm
Regional extent
Southwestern Gissar. corresponds to the "m" suite of S.N. Simakov (415) or beds with Inoceramus labiatus (114).
GeoJSON
Fossils
Belongs to the lower Turonian
Age
Depositional setting
Additional Information