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DarlaVolcanics Formation
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DarlaVolcanics Fm base reconstruction

DarlaVolcanics Fm


Period: 
Neoproterozoic

Age Interval: 
Ediacaran, 635 Ma


Province: 
N.India Lesser Himalaya

Type Locality and Naming

Simla (Shali Basin), named after Darla Village. [Original Publication: Srikantia, S. V. and Sharma, R.P. 1976. Geology of the Shali Belt and adjoining areas. Memoirs Geological Survey of India, 106 (1), 31-166.]

Synonym: Tattapani Volcanics


Lithology and Thickness

Mafic volcanics-slate.


Lithology Pattern: 
Volcanics


Relationships and Distribution

Lower contact

Nonconformable with Shali Gr (Bandia Fm)

Upper contact

Nonconformable with Basantpur Fm

Regional extent

From Tattapani in the Sutlej valley to Darla.


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[76.86,32.93],[76.28,33.02],[76.81,31.7],[77.38,30.95],[79.23,29.66],[80.13,29.32],[80.37,29.97],[79.78,30.1],[78.44,31.25],[77.6,31.59],[77.56,32],[76.86,32.93]]]]}}

Fossils

None


Age 

Martin (2017) projects as older than Mandhali

Age Span: 

    Beginning stage: 
Ediacaran

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
635.00

    Ending stage: 
Ediacaran

    Fraction up in the ending stage: 
0.2

    Ending date (Ma):  
615.76

Depositional setting

Submarine tholeiitic flows


Depositional pattern:  


Additional Information

Represents post Shali rifting


Compiler:  

O.N. Bhargava & Birendra Singh. Age estimates based on A.J. Martin, 2017. A review of Himalayan stratigraphy, magmatism, and structure. Gondwana Research 49 (2017) 42–80.