No CrossRef data available.
Article contents
A note on some garnetiferous biotite schists from Gangpur, Eastern India, and their polyphase metamorphism
Published online by Cambridge University Press: 01 May 2009
Summary
Textural features of two types of garnetiferous biotite-schists from the Iron-ore Series, Gangpur, developed at and near Potob, Ranchi District, indicate stages of development of the two rocks and their polyphase metamorphism.
- Type
- Articles
- Information
- Copyright
- Copyright © Cambridge University Press 1970
References
REFERENCES
Chatterjee, N. D. 1966. In Lotze, Fr. & Schmidt, K. (Eds.): Praekambrium Handbuch der stratigraphischen Geologie. Bd. XIII, pp. 343–388. Ferdinand Enke Verlag, Stuttgart.Google Scholar
Dunn, J. A. & Dey, A. K. 1942. The geology and petroglogy of Eastern Singhbhum and surrounding areas. Mem. geol. Surv. India 69, Pt. 2.Google Scholar
Johnson, M. R. W. 1963. Some time relations of movement and metamorphism in the Scottish Highlands. Geologie Mijnb. 42, 121–142.Google Scholar
Krishnan, M. S. 1933. The occurrence and distribution of staurolite in Gangpur State. Q. Jl geol. min. met. Soc. India 5, 67–74.Google Scholar
Naha, K. 1962. Time and place of progressive regional metamorphism: a study from the Precambrian of Eastern India. Geol. Rdsch. 52, 810–818.CrossRefGoogle Scholar
Sarkar, S. N. & Saha, A. K. 1962. A revision of the Precambrian stratigraphy and tectonics of Singhbhum and adjacent areas. Q. Jl geol. min. met. Soc. India, 34, 97–136.Google Scholar
Sarkar, S. N. & Saha, A. K. 1963. On the occurrence of two intersecting orogenic belts in Singhbhum and adjacent areas. Geol. Mag. 100, 69–92.CrossRefGoogle Scholar
Spry, A. 1963. Origin and significance of snowball structure in garnets. J. Petrology 4, 211–222.CrossRefGoogle Scholar
Thompson, J. B., Jr. 1957, The graphical analysis of mineral assemblages in pelitic schists. Am. Miner. 42, 842–858.Google Scholar