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Tirutturaipundi Formation
Click to display on map of the Ancient World at:
Tirutturaipundi Fm base reconstruction

Tirutturaipundi Fm


Period: 
Paleogene, Neogene

Age Interval: 
Oligocene-Early Miocene (late Paleogene-earliest Neogene); Subsurface – Nagapattinam sub-basin


Province: 
E.India Cauvery Basin

Type Locality and Naming

SUBSURFACE: The type section is located at exploratory well Tirutturaipundi-A (depth interval: 1000-365 m), on the Devakottai-Pattukottai Ridge of Nagapattinam subbasin. The hypostratotype is in the well PH-I-A (depth interval: 1271-435 m). It was named after the Tirutturaipundi village by ONGC team steered by Venkatarengan et al.(1993) and issued as Document-VII by KDMIPE, ONGC, Dehradun (1993).

[Figure 1: Type-section Map of Subsurface Formations]


Lithology and Thickness

Sandstone. Mainly sandstone with alternations of minor limestone beds. The sandstone is yellow to brown and gray, medium- to coarse-grained with floating pebbles, subangular to subrounded, moderate to poorly sorted and fossiliferous, with bands of light gray, compact siliceous limestone. Its thickness varies from 438-658 m. Part of Narimanam Gr.

[Figure 2: Generalized Stratigraphy and Petroleum System of Cauvery Basin (from dghindia.gov.in)]

[Figure 3: Generalized Stratigraphy of Cauvery Basin (Provided by A. Nallapa Reddy & R. Nagendra)]


Lithology Pattern: 
Sandstone


Relationships and Distribution

Lower contact

Unconformable with the Karaikal Fm / Tirupundi Fm / Kamalapuram Fm.

Upper contact

Conformable with the Madanam Fm /Tittacheri Fm.

Regional extent

It is present in the southern part of the Nagapattinam sub-basin extending towards the Palk Bay sub-basin, where its main depocenter lies.


GeoJSON

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Fossils

Myogipsinoides complanata-formosaensis, Nummulites fichteli, Globigerina sastrii and Chiliguembelina cubensis.


Age 

Oligocene (at least down into Rupelian implied by Chiliguembelina cubensis)-Early Miocene (late Paleogene-early Neogene)

Age Span: 

    Beginning stage: 
Chattian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
27.29

    Ending stage: 
Burdigalian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
15.99

Depositional setting

Inner-Middle neritic.


Depositional pattern:  


Additional Information

This litho-unit was first recognized by R. P. Rao et al. (1971)(Progress report on studies in Cauvery Basin (Field season 1) 70-71, unpublished ONGC report), and Venkatarengan et al. (1993) have adopted it later.


Compiler:  

A. Nallapa Reddy & R. Nagendra