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

Habur Fm


Period: 
Cretaceous

Age Interval: 
Albian


Province: 
NW.India Rajastan-Jaisalmer Basin

Type Locality and Naming

OUTCROP. Outcrop of Habur village and Kanoi village. [Original Publication: Swaminath, J., Krishnamurthy, J.G., Verma, K.K., and Chandak, G.J., 1959, General geology of Jaisalmer area, Rajasthan, ECAFE Symposium, Mineral Research and Development Series 10: 154-155]. Reference well: Outcrops near Kuchri and Kali Dungri areas. Well Bhuana-1, interval 400-603 m.

Synonyms: Oldham (1886) first described this formation as “Abur beds” and also mentioned its representative outcrops near Kuchri, Habur, Te-Takkar. Carter (1861) and Blanford (1877) also have mentioned about “Kuchri Ammonite Bank”. Swaminath et al., (1959) dropped the word “beds” and described this sequence as “Abur Formation” and the same has continued later (Dasgupta et al., 1973; Mishra et al.,1 993).


Lithology and Thickness

Sandy limestone. This formation comprises mainly alternations of calcareous sandstone and coquina limestone in the lower part, and foraminiferal limestone with shale interbeds in the upper part. Dasgupta et al. (1973) measured its thickness between 90-100 m along traverses in kali Dungri- Serawa, Kuchri and Te-Takkar areas. In subsurface, maximum thickness of the order of 203m has been recorded in the well Bhuana-1.

[Figure 1: Location map of West Rajasthan Basins (after Pandey and Dave, 1998)]

[Figure 2: Stratotype of Habur Fm, Mesozoic Lithostratigraphy of the Jaisalmer Basin, Rajasthan, Journal of the Paleontological Society of India, Vol. 51(2) (after Singh N.P, 2006)]


Lithology Pattern: 
Sandy limestone


Relationships and Distribution

Lower contact

The lower boundary between Habur Formation and underlying Pariwar Fm is in the scarp, east of Habur village, is disconformable with the presence of ironstone bands.

Upper contact

The upper boundary marks a major break between Mesozoic and Cenozoic sequences. It unconformably underlies Sanu Fm near Mohammad-ki-Dhani and Kali Dungri. Further in northwest the formation is directly overlain by Khuiala Fm.

Regional extent

[Figure 3: Stratigraphic Correlation of Rajasthan Basins (from dghindia.gov.in)]


GeoJSON

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Fossils

The lower part of this formation has yielded Ammonites.


Age 

Early Cretaceous (ca. 120 to 113 Ma?)

Age Span: 

    Beginning stage: 
Aptian

    Fraction up in beginning stage: 
0.9

    Beginning date (Ma): 
114.02

    Ending stage: 
Albian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
100.50

Depositional setting

Shallow inner neritic.


Depositional pattern:  


Additional Information


Compiler:  

D.S.N Raju