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Cenozoic
Cretaceous
Jurassic
Triassic
Permian
Carboniferous
Devonian
Silurian
Ordovician
Cambrian
Neoproterozoic


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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Zortashkol Limestone Formation
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Zortashkol Limestone Fm base reconstruction

Zortashkol Limestone Fm


Period: 
Cretaceous

Age Interval: 
Berriasian – Hauterivian (K2), Z1


Province: 
East Tajik (NE Pamir)

Type Locality and Naming

Synonym:

Reference section:


Lithology and Thickness

Limestone, sandstone, conglomerate at base. Thickness is 500-600 m.


Lithology Pattern: 
Sandy limestone


Relationships and Distribution

Lower contact

The schematic stratigraphic column indicates the next formation is Silty limestone

Upper contact

Regional extent

This unit is part of the Eastern Pamir Plateau. The Zortashkol thrust sheet (sometimes called the Zortashkul nappe) lies in the Rangkul–Shorkul area, NE Tajikistan, not far from the Karakul basin.


GeoJSON

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Fossils

fossil algae


Age 

The stratigraphic age of the ~2.5 km thick strata of the Tuzguny-Terezki and Zortashkol thrust sheets - based on fossil algae is debated; Dronov et al. [2006] suggested a Meso-Neoproterozoic (Riphean) age; Vlasov et al. [1991] posited a Cambrian-Silurian age. The youngest detrital Zrn U-Pb age group of ~605 Ma in one sample supports the presence of Ediacaran strata. The Zortashkol thrust sheet contains >3 km of Silurian to Cretaceous strata. Strata that unconformably cover the Tuzguny-Terezki and Zortashkol thrust sheets were originally classi ed as Cretaceous and Paleogene [Yushin et al., 1964] but revised to Cretaceous by Vlasov et al. [1991]. Dronov et al. [2006] questioned all evidence for Paleogene deposits. (Rutte et al., 2017) Hence adjusted in Berriasian – Hauterivian for schematic stratigraphic column purpose.

Age Span: 

    Beginning stage: 
Berriasian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
143.10

    Ending stage: 
Hauterivian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
126.50

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Extracted from Rutte, D., L. Ratschbacher, S. Schneider, K. Stübner, M. A. Stearns, M. A. Gulzar, and B. R. Hacker (2017), Building the Pamir-Tibetan Plateau—Crustal stacking, extensional collapse, and lateral extrusion in the Central Pamir: 1. Geometry and kinematics, Tectonics, 36, 342–384, doi:10.1002/2016TC004293.