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Isalo Gr

Isalo Gr


Period: 
Triassic, Jurassic

Age Interval: 
Late Triassic-Middle Jurassic (Carnian-Bathonian)


Province: 
Madagascar

Type Locality and Naming

Morondava Basin and Majunga Basin (Madagascar). Named for regions in Madagascar. It represents the major Late Triassic to Early Jurassic depositional sequence within the Malagasy rift basins. It is often subdivided into units such as Isalo I and Isalo II. Includes in Stormberg Gr in Morondava Basin (Madagascar)

Synonym:


Lithology and Thickness

The group is characterized largely by coarse clastic sequences, predominantly fluvial conglomerates and sandstones.


Lithology Pattern: 
Fine-grained sandstone


Relationships and Distribution

Lower contact

The Isalo Group (specifically the medial Isalo II in the Morondava Basin) possesses a marked basal unconformity, overstepping older Karoo strata directly onto the Precambrian basement. Regionally, it rests above the Upper Sakamena Gr.

Upper contact

Conformably to unconformably succeeded by transgressive marine Liassic (Early Jurassic) deposits.

Regional extent

Found within the Karoo-aged rift basins of Madagascar, specifically the Morondava Basin in the south and the correlated Majunga Basin to the north. Stormberg Gr equivalent in Madagascar.


GeoJSON

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Fossils


Age 

Late Triassic-Middle Jurassic (Carnian-Bathonian)

Age Span: 

    Beginning stage: 
Carnian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
237.00

    Ending stage: 
Bathonian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
165.29

Depositional setting

Fluvial environments with marginal marine influences.


Depositional pattern:  


Additional Information

In the Majunga Basin to the north, Isalo I appears to be the Stormberg Gr-equivalent unit, whereas in the Morondava Basin, Isalo II is considered the equivalent.


Compiler:  

From the O. Catuneanu et al. The Karoo basins of south-central Africa, Journal of African Earth Sciences 43 (2005) 211–253; Pique´, A., et al. (1999): L'ouverture et le de´veloppement du bassin de Morondava... Journal of African Earth Sciences.