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Pandey, Shivani
- Devonian Ichnofossils from the Farakah Muth Section of the Pin Valley, Spiti Himalaya
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1 Wadia Institute of Himalayan Geology, 33 General Mahadeo Singh Road, Dehradun - 248 001, IN
1 Wadia Institute of Himalayan Geology, 33 General Mahadeo Singh Road, Dehradun - 248 001, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 78, No 3 (2011), Pagination: 263-270Abstract
The Muth Formation is one of the most characteristic marker horizon traced throughout the northwestern Himalaya. The present studies were carried out in the Farakah Muth (Pin Valley) section of Spiti Basin. The formation uniformly consists of quartzarenite with a high textural and compositional maturity. The development of carbonate beds in the upper part of the Muth Formation separates it conformably from the overlying Lipak Formation. A variety of traces were observed throughout the succession, includes: Metaichna, Planolites, Skolithos, vertical and horizontal burrows. The presence of ichnofossils in the Muth Formation of the Farakah section indicates subtidal settings having soft sandy substrate, whereas, the gradual maturity of the quartz grains from base to top indicates deposition under high energy condition.Keywords
Ichnofossils, Depositional Environment, Muth Formation, Pin Valley, Spiti Himalaya.
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