Mandhali Fm
Type Locality and Naming
Himachal Pradesh-Uttarakhand, Deoban Basin. Named after the village Mundali, nestling in the Deoban mountain in the Bawar pargana (northern Chakarata area) of Kumaun region. [Original Publication: Oldham, R.D. (1883). Note on the Geology of Jaunsar and Lower Himalaya. Record Geological Survey of India, 16, 193-198.]
Lithology and Thickness
Conglomerate. Conglomerate, shale, siltstone, limestone, dolostone; 800 m in Deoban Basin. Limestone. Grayish green and black carbonaceous pyritic phyllites or slates interbedded and interbedded plastically folded blue-banded limestones and a variety of paraconglomerates; ~400 m in Kumaun Region.
Relationships and Distribution
Lower contact
Unconformable with of r in Deoban Basin, Discordant contact with Deoban Gr in the type area Tons valley, but with break or unconformity elsewhere in Kumaun Region.
Upper contact
Conformable with Chandpur Fm in Deoban Basin. The upper limit of the Mandhali in the Krol Nappe is marked by gradational passage into the Chandpur Fm above (Auden, 1934), and the upper limit has been placed arbitrarily at the top of the Bansa Limestone by Auden in Kumaun Region.
Regional extent
Eastern Himachal and western Uttarakhand. Some workers correlated it with the Baliana (Blaini) Fm, now correlated with the Basantpur Fm.
GeoJSON
Fossils
None in Deoban Basin. In Kumaun Region, Stromatolites: Jurusania, Collenia parva (Valdiya, 1969a) Osagia tenuilamellata (Nalivikin, 1966), Jurusania himalayica, Irregularia (Stromatolitic forms) Sinha (1977)
Age
Depositional setting
Marine, shallow-subtidal
Additional Information
Sor slate and Thalkedar limestone are units of this Formation in Kumaun Region.