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Paniam Quartzite Formation
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Paniam Quartzite Fm base reconstruction

Paniam Quartzite Fm


Period: 
Tonian

Age Interval: 
Late Tonian


Province: 
Proterozoic S.India – Cuddapah basin

Type Locality and Naming

Middle-upper formation (4 of 6) of Kurnool Gr.

Synonyms: Plateau Quartzite or Pinnacled Quartzite because of the special geomorphic features in the Kumool district.


Lithology and Thickness

Sandstone: The bulk is very well-sorted quartz arenite. Amalgamated wavy planar to lenticular beds give rise to meter-thick sheet like geometry. Wavy planar laminations, trough cross-strata,

and large planar tabular cross-strata are common in the quartz arenite (Fig. image G).

[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: 
Sandstone


Relationships and Distribution

Lower contact

Underlain by Owk Shale Fm with a transition zone marked by thin, wavy bedded to rippled, medium-grained quartzite (Fig. image F).

Upper contact

Regional extent


GeoJSON

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Fossils


Age 


Age Span: 

    Beginning stage: 
Tonian

    Fraction up in beginning stage: 
0.8

    Beginning date (Ma): 
776.00

    Ending stage: 
Tonian

    Fraction up in the ending stage: 
0.82

    Ending date (Ma):  
770.40

Depositional setting

Shallow-marine, bars with macrotidal influence. Very well-sorted quartz arenite with amalgamated cross-stratified beds have been interpreted as products of wave reworked bars in a near-shore open environment


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.