Para Fm
Type Locality and Naming
Spiti Valley. [Original Publication: Stoliczka, F. 1865. Geological section across the Himalayan mountain range from Wangtu Bridge on the river Sutlej to Sungdeo with an account of formations in Spiti accompanied by a revision of all known fossils from that district. Memoirs of Geological Survey of India, 5: 153p]
[Figure: Zanskar-Spiti-Kumaun region location (provided by Om Bhargava)]
Synonyms: lower part of Kioto Limestone (Hayden, 1904); Kioto Group
[Figure 0: History of Triassic lithostratigraphic nomenclature of Spiti (after Bhargava et al., 2004)]
Lithology and Thickness
Limestone. Gray, thin to medium-bedded limestone in basal part, in upper part dolomite predominates. 150 m,
Relationships and Distribution
Lower contact
Lower contact with the Nunuluka Fm is conformable.
Upper contact
Gradational contact with the overlying Tagling Fm is gradational.
Regional extent
Zanskar-Spiti and Himachal Pradesh to Kumaun-Garhwal region of Northwest Tethyan Himalaya
GeoJSON
Fossils
Megalodon ladakhensis, Entolium cf. subdemissum, Petcen chabrangensis, Lima cumaunica, Diceracardium himalayaensis, Spirigera noetlingi
Age
Depositional setting
Storm dominated winnowed shelf edge sand area with tidal channels and partly in shoal area (Bhargava, 2008).
Additional Information