Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Manjari Pathak"'
Publikováno v:
Environmental Challenges, Vol 9, Iss , Pp 100609- (2022)
In the Central Himalaya, the Kali River flow through the rocks of Tethys sedimentary (TS) sequences and Higher Himalayan crystallines (HHC) towards the upstream and through the Lesser Himalayan metasedimentary (LHS) the Siwaliks rocks in the downstre
Externí odkaz:
https://doaj.org/article/7472edfb4d4345aebf52638e7d877591
Autor:
Santosh Kumar, Shailendra Pundir, Vikoleno Rino, Sita Bora, Manjari Pathak, null Anettsungla, Hansa Joshi, Manohar Singh Rawat, Thepfuvilie Pieru, Kh. Mohan Singh
Publikováno v:
Geological Journal. 57:1476-1510
Autor:
Manjari Pathak, Santosh Kumar
Publikováno v:
Geological Society, London, Special Publications. 481:341-377
Autor:
Vikoleno Rino, Santosh Kumar, Shunmugam Raju, Manjari Pathak, Yasutaka Hayasaka, Kosuke Kimura, Kentaro Terada
Publikováno v:
Lithos. 277:356-375
The Meghalaya Plateau and the Mikir Hills constitute a northeastern extension of the Precambrian Indian Shield. They are dominantly composed of Proterozoic basement granite gneisses, granites, migmatites, granulites, the Shillong Group metasedimentar
Autor:
Santosh Kumar, Manjari Pathak
Publikováno v:
Journal of the Geological Society of India. 75:715-730
Felsic magmatic rocks in Kameng corridor of western Arunachal Himalaya are represented by extensively exposed Palaeoproterozoic porphyritic muscovite-biotite granite (GGn) of the Bomdila Group and small stock-like Mesoproterozoic hornblende-biotite g
Publikováno v:
Journal of the Geological Society of India. 75:539-548
Late Archaean to Palaeoproterozoic felsic magmatic lithounits exposed in the central part of the Bundelkhand massif have been mapped and their redox series (magnetite vs ilmenite series) evaluated based on magnetic susceptibility (MS) data. The centr
Autor:
Manjari Pathak, Santosh Kumar
Publikováno v:
Himalayan Journal of Sciences. 5:132
DOI = 10.3126/hjs.v5i7.1316 Himalayan Journal of Sciences Vol.5(7) (Special Issue) 2008 p.132