Home Multi-Country Search About Admin Login
Cenozoic
Cretaceous
Jurassic
Triassic
Permian
Carboniferous
Devonian
Early Paleozoic

Search by
Select Region(s) to search
Hold Ctrl (Windows/Linux) or Command (Mac) to select multiple
Soltanieh Formation
Click to display on map of the Ancient World at:
Soltanieh Fm base reconstruction

Soltanieh Fm


Period: 
Cambrian,

Age Interval: 
Ediacaran – Cambrian Stage 2, Ir4


Province: 
Iran

Type Locality and Naming

Column: Iran NW - Alborz

Synonym:


Lithology and Thickness

It is further divided into Upper Dolomite Mbr, Upper Shale Mbr, Middle Dolomite Mbr, Lower Shale Mbr, Lower Dolomite Mbr. Thick dolomite unit that forms cliffs in the Soltanieh region of Iran. Over 100m thick, this formation consists of three units: a lower dolomite member which is yellow, well-bedded, and full of chert nodules. The middle Chapoghlu member consists of greenish grey agrilliceous shales and slates. The upper dolomite unit is massive, light gray with common black chert nodules throughout. Stromatolites are fairly common in this formation.


Lithology Pattern: 
Coarse-grained Sandstone


Relationships and Distribution

Lower contact

Regionally, the schematic strat column indicates the next older unit as Bayandor Fm

Upper contact

Regionally, the schematic strat column indicates the next younger unit as Barut Fm

Regional extent


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[61.01,35.91],[56.79,36.94],[52.22,35.37],[47.84,37.15],[46.78,36.27],[47,34.85],[51.69,31.89],[60.86,34.79],[61.01,35.91]]]]}}

Fossils


Age 

Ediacaran – Cambrian Stage 2

Age Span: 

    Beginning stage: 
Ediacaran

    Fraction up in beginning stage: 
0.8

    Beginning date (Ma): 
558.04

    Ending stage: 
Cambrian Stage 2

    Fraction up in the ending stage: 
0.3

    Ending date (Ma):  
526.60

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Middle East Geological Timescale 2008 Al-Husseini, Journal of Middle East Petroleum Geosciences v 13, no. 4