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Papan Formation

Papan Fm


Period: 
Neogene

Age Interval: 
upper Pliocene (Piacenzian), F1


Province: 
Fergana

Type Locality and Naming

By the village of Papan, Fergana, Kyrgyzstan. A.S. Telenkov, 1964 (468, p.84). The stratigraphic name is used limitedly.

Synonym: Papan Suite, Папанская св.

Reference section:


Lithology and Thickness

Reddish sandstones, siltstone (aleurolites), gravelites, conglomerates. Thickness 40-878m.


Lithology Pattern: 
Sandstone


Relationships and Distribution

Lower contact

Lies unconformably on the Kaplankul Fm or Aldyr Fm

Upper contact

Overlain unconformably by the Akburin Fm

Regional extent

Fergana. Corresponds to the brown suite. In the 1st scheme of N.P. Vasilkovsky (126). Correlated with the Akchop suite of NW Fergana and the Tavildar suite of Darvaz (Tajikistan), (166)


GeoJSON

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Fossils

Contains ostracods - Eucypris pursugolensis Manel., E. vitabianus Schn., rhinoceros’ bones, hare, rodents, mastodon, hare, spores, and pollen.


Age 

Age - early and middle Pliocene. B. I. Pinhasov refers to the late Pliocene. For schematic stratigraphic column representation, it is considered Piacenzian.

Age Span: 

    Beginning stage: 
Piacenzian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
3.60

    Ending stage: 
Piacenzian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
2.58

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

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