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Tindara Formation
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Tindara Fm base reconstruction

Tindara Fm


Period: 
Triassic

Age Interval: 
Spathian


Province: 
NW Himalaya Kashmir Basin

Type Locality and Naming

The type section is in Tindara hillock in Pulwama district, Kashmir. [Original Publication: Middlemiss, C.S. 1910. A revision of Silurian-Trias sequence in Kashmir. Record Geological Survey of India, 40(3): 206-260.]


Lithology and Thickness

Limestone. The Tindara Formation is composed of nodular limestone with minor shale.


Lithology Pattern: 
Limestone


Relationships and Distribution

Lower contact

Overlies Khunamuh Fm.

Upper contact

Underlies Khreuh Fm

Regional extent

Kashmir Basin


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[76.46,33.21],[75.58,34.05],[74.97,34.3],[74.17,34.3],[74.09,33.87],[74.39,33.24],[75.71,32.87],[76.46,33.21]]]]}}

Fossils

Conodont: Neospathodus timorensis


Age 

Regarded to represent Spathian substage; but N. timorensis implies basal Anisian also.

Age Span: 

    Beginning stage: 
Olenekian

    Fraction up in beginning stage: 
0.3

    Beginning date (Ma): 
248.93

    Ending stage: 
Anisian

    Fraction up in the ending stage: 
0.2

    Ending date (Ma):  
245.65

Depositional setting

The Tindara Formation was mainly deposited below wave base.


Depositional pattern:  


Additional Information


Compiler:  

O.N. Bhargava & Birendra Singh