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

Godhara Fm


Period: 
Neogene

Age Interval: 
Aquitania to Lower Burdigalian (Miocene)


Province: 
W.India Kutch Basin

Type Locality and Naming

SUBSURFACE. Interval 850-2049m in well SP-1-1. [Original Publication: Zutshi, P.L., Mittal, S.K and Shah, L. (1993) Lithostratigraphy of Indian Petroliferous Basins, Document IV, Kutch Saurashtra Basin, KDMIPE, ONGC Publication, pp 1-50.]

[Fig. Geological and structural map of Kutch, also showing the onshore and offshore wells drilled for oil exploration. (Map by Rasoul Sorkhabi in GeoExpro Dec2014, based on various sources including S.K. Biswas, Current Science, 25May2005)]


Lithology and Thickness

Shallow-marine marl. It consists of shale/claystone/limestone alternations and minor sandstones. 1200 m in well SP-1-1, thickness increases towards west.

[Figure 1: Seismic section showing Middle Miocene, Early Eocene and Paleocene plays (after Bhowmick and Vasudevan, 2013)]


Lithology Pattern: 
Shallow-marine marl


Relationships and Distribution

Lower contact

Unconformable with the Narayan Sarovar Fm (?; next older subsurface unit seems to be the Mit Nadi Fm). It is marked by sharp break in resistivity and gamma rays logs. It also coincides with the top of M. complanata.

Upper contact

Conformable with the overlying Chassara Fm. It is marked at the end of limestone/claystone alternations to dominantly final clastic of Chassara Fm.

Regional extent


GeoJSON

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Fossils

Miogypsina (Miogypsinoides) dehaarti, M (L) excentrica, M. tani, M.(L) thecideaeformis


Age 

Aquitanian to Lower Burdigalian (Miocene)

Age Span: 

    Beginning stage: 
Burdigalian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
20.45

    Ending stage: 
Burdigalian

    Fraction up in the ending stage: 
0.25

    Ending date (Ma):  
19.34

Depositional setting

Deposited in inner shelf environment


Depositional pattern:  


Additional Information


Compiler:  

D.S.N Raju