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Moabund Formation

Moabund Fm


Period: 
Cretaceous

Age Interval: 
Maastrichtian.


Province: 
North East Basins of India

Type Locality and Naming

Type section is in the Well Deragon-1. Interval is from 1252 to 1690 m and 438 m thickness. Khanna and Srinivasachari (1973) designated this units as a sequence of shales with intercalated sandstones encountered in the well Dergaon-1, present between the overlying Tura Fm, (Pandey and Dave, 1998). [Original Publication: Khanna and Srinivasachari, (1973). Well completion report of Degaon – 1, unpublished report of ONGC.]. Reference section: Um Sorhyngkew River Section, its thickness is 151 m.

[Figure 1: Formation stratotypes of North East Basins (modified after Pandey and Dave, 1998)]


Lithology and Thickness

Sandy claystone. In the type section Well Dergaon – 1, it comprises greenish grey, jointed shales with intercalated sandstones and calcareous veins. Cores indicate the presence of non-calcareous mudstones with incipient development of fissility. The sandstones are fine to very fine grained and exhibit lenticular bedding.


Lithology Pattern: 
Sandy claystone


Relationships and Distribution

Lower contact

It unconformably overlies the sandstone-dominated sequence of the Bamangaon Fm.

Upper contact

It is unconformably overlain by the Tura Fm.

Regional extent

Dhansiri Valley.


GeoJSON

null

Fossils


Age 

Maastrichtian.

Age Span: 

    Beginning stage: 
Maastrichtian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
72.17

    Ending stage: 
Maastrichtian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
66.04

Depositional setting

It is interpreted to have been deposited mostly in an outer shelf environment.


Depositional pattern:  


Additional Information


Compiler:  

D.S.N Raju