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Owk Shale Formation
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Owk Shale Fm base reconstruction

Owk Shale Fm


Period: 
Tonian

Age Interval: 
Late Tonian


Province: 
Proterozoic S.India – Cuddapah basin

Type Locality and Naming

Lower-middle formation (3 of 6) of Kurnool Gr


Lithology and Thickness

Claystone: Color laminated shale with minor felsic volcaniclastics; only 10-12 m thick. It consists of red and brown weathering, thinly laminated shale (Fig. image E) with a 2-m-thick zone in the lower part which includes intercalation of ochreous shale and more compact cm thick welded coarse to fine rhyolitic to rhyodacitic tuff and volcaniclastic sandstone layers. Some of the tuffaceous horizons also show ferruginous enrichment. The shale beds have plane parallel laminations.

[Field photographs showing lithology and sedimentary features in the Kurnool Group. Banganapalle Quartzite Fm – (A) basal conglomerate of overlying granitic basement, and (B) thick matrix supported polymict conglomerate with apparent size grading. Narji Limestone Fm - (C) lower part with thin wavy bedded impure limestone, and (D) glauconitic sandstone interbeds in limestone; note pockets of lime pebble conglomerate. Owk Shale Fm - (E) Thinly laminated ash beds, and (F) transition from Owk Shale (lower half of photo) to Paniam Quartzite Fm. Paniam Quartzite Fm - (G) truncated wavy lamination. Koilkuntla Limestone Fm - (H) thin bedded argillaceous limestone, and (I) impure limestone-shale intercalation within the Koilkuntla Limestone Fm to Nandyal Shale Fm transition. (from Saha et al., 2016)]


Lithology Pattern: 
Claystone


Relationships and Distribution

Lower contact

Underlain by Narji Limestone Fm with a sharp transition that is commonly marked by a clayey horizon.

Upper contact

Graded upward into the Paniam Quartzite Fm with a transition zone marked by thin, wavy bedded to rippled, medium-grained quartzite and commonly marked by a clayey horizon (Fig. image F).

Regional extent

Laterally extensive across the Kurnool district


GeoJSON

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Fossils


Age 


Age Span: 

    Beginning stage: 
Tonian

    Fraction up in beginning stage: 
0.77

    Beginning date (Ma): 
784.40

    Ending stage: 
Tonian

    Fraction up in the ending stage: 
0.8

    Ending date (Ma):  
776.00

Depositional setting

Outer shelf


Depositional pattern:  


Additional Information


Compiler:  

From: Saha D. (Dilip), Patranabis-Deb, S., and Colllins, A.S. (2016) Proterozoic stratigraphy of southern Indian cratons and global context. In: Stratigraphy & Timescales, 1: 1-59.