Beshkap Fm
Type Locality and Naming
Includes in Hisar-Zarafshan ranges, and Obisafit, Turkparidin, Chakykalya typesections
(Dzhalilov et al., 1971)
Synonym: Beshkapskaya suite, бешкапинская свита
Reference section:
Lithology and Thickness
It is composed of greenish-gray sandstones and siltstones with layers of limestone. The thickness is 10-14 m.
In regions Turkestan, Zarafshan-Gissar, South Gissar, Karategin, Dushanbe, Qafirnigan, Vakhsh, Zaalai and Darvaz districts, the considered horizon corresponds to the Shirabad Fm (Andreeva, 1966), composed of gypsums with interlayers of red-colored argillaceous siltstones.
Relationships and Distribution
Lower contact
At the base of the suite, there are massive gray-green sandstones. They conformably or with slight erosion overlie the deposits of Berriasian, Middle Aptian or Upper Hauterivian - Middle Aptian.
Upper contact
At the top of the suite, there are massive gray-green sandstones. They are conformably overlain by the deposits of the Cenomanian and Turonian.
Regional extent
In regions Turkestan, Zarafshan-Gissar, South Gissar, Karategin, Dushanbe, Qafirnigan, Vakhsh, Zaalai and Darvaz districts, the considered horizon corresponds to the Shirabad Fm (Andreeva, 1966).
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Fossils
Age
Depositional setting
Additional Information