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

Batal Fm


Period: 
Ediacaran, Cambrian

Age Interval: 
?Precambrian-Lower Cambrian


Province: 
NW Himalaya Zanskar-Spiti

Type Locality and Naming

Type section is in Batal village in the Chandra Valley, Lahaul-Spiti region, Himachal Pradesh

[Original Publication:s Srikantia, S. V., Ganesan, T. M., Sinha, P. K. and Tirkey, B. 1976. Geology of Part of Zanskar Mountains, Ladakh Himalaya with special reference to late Caledonian “Kurgiakh Orogeny”. “Geology, Mineral Resources and Natural Resources of Power Development of Himalayas with particular Reference to Kashmir”. Geological Survey of India, Abstracts, 1–3. Srikantia, S.V., 1981. The lithostratigraphy, sedimentation and structure of Proterozoic–Phanerozoic formations of Spiti basin in the higher Himalaya of Himachal Pradesh, India. In: Sinha, A.K. (Ed.), Contemporary Geoscientific Researches in India (a commemorative volume in honor of S.P. Nautiyal). Bishen Singh Mahendra Pal Singh, Dehra Dun, pp. 31–48; Srikantia, S.V., Ganesan, T.M., Rao, P.N., Sinha, P.K., Turkey, B., 1979. Geology of Zanskar area, Ladakh Himalaya. Himalayan Geology 8 (2), 1009–1033.] [Nanda, M.M. and Singh, M.P. (1977) Stratigraphy and sedimentation of the Zanskar area, Ladakh and adjoining parts of the Lahaul region of Himachal Pradesh. Him. Geol., v.6, pp.365-388].

Synonyms: Phe Formation (Nanda and Singh, 1977)

[Figure: Zanskar-Spiti-Kumaun region location (provided by Om Bhargava)]


Lithology and Thickness

Clayey sandstone. Comprised of micaceous quartzite with pyritous carbonaceous phyllite, olive green slate and coarse sandstone (Srikantia, 1981). Type section (> 2000 m). Bhargava et al (1991) description: Quartzite, medium to fine grained, made up of subangular to subrounded quartz grains in chloritic matrix. Pebble bed having rounded flat pebbles/granules of quartzite and vein quartz. Slate to schist, slate in claystone matrix. Carbonaceous shale. Basic volcanics in basal part.

[Figure 1: Field photograph showing the rocks of Batal Formation near the Batal Bridge, in Chandra Valley Lahaul-Spiti.]


Lithology Pattern: 
Clayey sandstone


Relationships and Distribution

Lower contact

In Spiti region its lower contact with underlying Salkahal Gr (Group) is a recognizable contact.

Upper contact

Its upper contact with overlying Kunzam La Fm is gradational, locally tectonic.

Regional extent

Zanskar-Spiti and Himachal Pradesh to Kumaun-Garhwal region of Northwest Tethyan Himalaya

[Figure: Paleozoic successions of Himalayas West-to-East (after Bhargava, 2008)]


GeoJSON

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Fossils

Acritarch (Vendian: Anguloplanian sp.; and Pulvinomorpha sp) (Kumar et al., 1984)


Age 

Latest Precambrian- ?Early Cambrian [For graphics, base put as 80% up in Ediacaran; and conformable gradiational contact to Kunzam La Fm sets the top]

Age Span: 

    Beginning stage: 
Ediacaran

    Fraction up in beginning stage: 
0.8

    Beginning date (Ma): 
558.04

    Ending stage: 
Cambrian Stage 4

    Fraction up in the ending stage: 
0.5

    Ending date (Ma):  
511.75

Depositional setting

Metamorphosed sediments.


Depositional pattern:  


Additional Information


Compiler:  

O.N. Bhargava & Birendra Singh.