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Main source = Baratov, R.B., et al. (1976). Subdivisions of stratified and intrusive rocks of Tajikistan. Publishing House "Donish", Dushanbe, 269 pp. plus tables. Provided by Dr. Jovid Aminov, Nazarbayev University, Astana, Kazakhstan Translated to English by the GeoGPT group, Zhejiang Lab, Hangzhou, China--see About

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Rawait Formation
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Rawait Fm base reconstruction

Rawait Fm


Period: 
Cretaceous

Age Interval: 
Middle Albian (K12), C1, C1a, C1b, C1c


Province: 
Central W Tajik

Type Locality and Naming

Includes in Hisar-Zarafshan ranges, and Obisafit, Turkparidin, Chakykalya typesections

(Dzhalilov et al., 1971)

Synonym: Babatag horizon, Бабатаrскому горизонту, Rawait suite

Reference section:


Lithology and Thickness

It is composed of freshwater concretionary limestones and red-colored conglomerates, sandstones, and clays, with a total thickness of 35 m.


Lithology Pattern: 
Sandy limestone


Relationships and Distribution

Lower contact

They conformably or with slight erosion overlie the deposits of Berriasian, Middle Aptian or Upper Hauterivian - Middle Aptian.

Upper contact

They are conformably overlain by the deposits of the Cenomanian and Turonian.

Regional extent

It is distributed in the Zeravshan-Gissar region. Co-eval with Babatag Fm


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[67.98,38.93],[67.84,38.93],[67.75,39],[67.69,39.14],[67.95,39.18],[68.65,39.29],[70.55,39.46],[70.71,39.43],[70.66,39.23],[70.01,38.98],[69.39,38.86],[68.77,38.75],[68,38.7],[67.98,38.93]]]]}}

Fossils

Rhynocypris gissarensis Andrv


Age 

Middle Albian

Age Span: 

    Beginning stage: 
Albian

    Fraction up in beginning stage: 
0.35

    Beginning date (Ma): 
108.76

    Ending stage: 
Albian

    Fraction up in the ending stage: 
0.6

    Ending date (Ma):  
105.58

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Extracted from Baratov, R. B. (1976). Subdivisions of stratified and intrusive rocks of Tajikistan. Donish, Dushanbe, 276.