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Main source = Abduazimova, Z.M. (Ed.), 2001. Stratigraphic Dictionary of Uzbekistan. IMR (Institute of Mineral Resources), Tashkent, 580 pp. (In Russian) Translated to English by the GeoGPT group, Zhejiang Lab, Hangzhou, China--see About

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Khavzak Formation

Khavzak Fm


Period: 
Devonian

Age Interval: 
Lochkovian, Z1


Province: 
Zarafshan-N.Gissar

Type Locality and Naming

Along the Havzak River, Arg Basin, Central Tajikistan. A.I. Lavrushevich, V.I. Lavrushevich, 1972 (262, p. 63). Stratotype along the Havzak River. Previously considered as the Upper Arg sub-suite. Upper formation in Arg Gr.

Synonym: Havzak Suite, Хавзакская св.


Lithology and Thickness

Dark gray to black, layered to massive, variably dolomitized limestones. Thickness is 150 m.


Lithology Pattern: 
Dolomitic limestone


Relationships and Distribution

Lower contact

It lies conformably on the Kupruk Fm

Upper contact

Conformably overlies the Bursyhirman Horizon in the Obisafy type of sections, the Turkparidin - Turkparidin Fm, the Chakylkalyan Fm - Akbasay Fm.

Regional extent

Zarafshan-Gissar mountain region.


GeoJSON

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Fossils

Contains tabulates - Favosites socialis Sok. et Tes., Pachyfavosites kozlowskii Sok.; rugosans - Tryplasma aequabilis Lonsd., Chavsakia chavsakiensis Lavrus., Holmophyllum taltiense Nikol., Strephophyllum turkparidense Lavrus., brachiopods - Lissotrypa alexandria Nikif., L. nasa Nikif., L. caudota Nikif., Retzia (?) argensis Nikif.


Age 

It belongs to the Zhdinian stage (379). A.I. Lavrushevich." Stratigraphic Lexicon (443). In the modern understanding - to the Lochkovian stage.

Age Span: 

    Beginning stage: 
Lochkovian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
419.00

    Ending stage: 
Lochkovian

    Fraction up in the ending stage: 
0.5

    Ending date (Ma):  
415.70

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Z.M. Abdazimova – In: GeoGPT translation of: “Abduazimova, Z.M. (Ed.), 2001. Stratigraphic Dictionary of Uzbekistan. IMR (Institute of Mineral Resources), Tashkent, 580 pp. (In Russian)”