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Bolgalin Formation

Bolgalin Fm


Period: 
Carboniferous

Age Interval: 
Moscovian, CK8, CK9


Province: 
Chatkal-Kuramin Region

Type Locality and Naming

Along the Chashly River, Karamazar Mountains. A.B. Dzainukov, M.E. Zaprozetov, V.N. Tkachev (V.N. Tkachev et al., 1988). In the territory of Tajikistan - Chashlinskaya, in Uzbekistan - Bolgaliinskaya suite. Stratotype of C. suite - Altyntopkan region, and B. suite - Belyauty region (Tashtepinsky heights on the southwestern subsidence of the Chatkal range).

Synonym: Bolgalinskaya (Chashlinskaya) Suite, Bolgalian, Болгалинская (чашлинская) св.


Lithology and Thickness

Fills volcano-tectonic grabens (Almalyk, Altyntopkan, Kurusay-Jangalik, and Shavaz-Dukent) and is exposed in the form of small fragments at the edges of ring structures (Lashkerek, Kyzylnurin, etc.). V.A. Arapov (64) identifies three subdivisions: lower (only in the Altyntopkan graben) - andesite tuffs, replaced by a layer of interbedded arkosic sandstones, conglomerates, siliceous shales, and rhyolite tuffs. Thickness 140-480m; middle - uniform fine- to medium-porphyritic andesites and trachyandesites, less frequently basalts, andesitic-basalts. Lava flows alternate with tuff layers, locally with conglomerate, sandstone, and siltstone (aleurolite) layers. Along with cover facies, this part of the section is associated with subvolcanic bodies of trachyandesites, monzonitoids. Thickness 120-500m; upper - agglomerate and block tuffs and xenotuffs, higher up – andesitic-dacite lavas. Thickness 145 665m. Total Thickness 1100m.


Lithology Pattern: 
Volcanics


Relationships and Distribution

Lower contact

Lies on a deeply eroded surface of older formations: Middle Devonian-Lower Carboniferous limestones; Lower-Middle Devonian volcanics; granitoids of the Karamazar Gr

Upper contact

Overlain with erosion by the Akchin Fm and younger formations.

Regional extent

Widely developed in the Kuramin and Chatkal ranges. L.I. Savitskaya et al. (450) describe a plant complex from the sedimentary layer of Kandyrkaya as part of the lower sub-suite of the Nadak Fm. Previously, in the territory of Uzbekistan, it was identified as the lower sub-suite of the Akchin Fm, and in Tajikistan - as the Minbulak Fm or Akchin Fm


GeoJSON

null

Fossils

Contains plant remains - Lepidodendron ex gr. lycopodioides Sternb., Calamites ex gr. sachsei Stur., Neuropteris heterophylla Brongn., N. ex gr. tenuifolia (Sloth.), Aulacotheca kandyrica Sav., Trigonocarpus sp., Cordaites ex gr. principalis (Germ.), Kandyrica vasilkovskyi (Sixt.), Ranczenkoella kandyrensis (Sixt.), Samoropsis sp., Cordaicarpus sp.


Age 

Age - Moscovian epoch of the Middle Carboniferous (460).

Age Span: 

    Beginning stage: 
Moscovian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
315.15

    Ending stage: 
Moscovian

    Fraction up in the ending stage: 
0.5

    Ending date (Ma):  
311.09

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

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