Hostname: page-component-76fb5796d-qxdb6 Total loading time: 0 Render date: 2024-04-29T05:57:07.517Z Has data issue: false hasContentIssue false

Ultramafic volcaniclastics of the Precambrian Dalma Volcanic Belt, Singhbhum, Eastern India

Published online by Cambridge University Press:  01 May 2009

A. Gupta
Affiliation:
80 Circular Road, Dinapore, Cantonment, India
A. Basu
Affiliation:
80 Circular Road, Dinapore, Cantonment, India
P. K. Ghosh
Affiliation:
Department of Geology, University of Patna, Patna, India

Summary

The Dalma volcanic belt in the Precambrian Eastern Indian shield is composed of a thick sequence of volcani-sedimentary assemblage with a group of predominantly ultramafic volcaniclastics having komatiitic chemistry. A volcanic origin is suggested by textural relationships and mineralogical composition, together with the presence of devitrified glass shards; these rocks are now mostly chlorite-tremolite schist.

Type
Articles
Copyright
Copyright © Cambridge University Press 1982

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Bhattachariya, D. S. & Das Gupta, D. 1979. Chemical clues to the origin of basic fragments embedded in a basaltic suite of the Precambrian metamorphic terrain of Singhbhum, E. India. Contr. Miner. Petrol. 71, 177–83.Google Scholar
Brooks, C. & Hart, S. R. 1974. On the significance of komatiite. Geology 2, 107–10.2.0.CO;2>CrossRefGoogle Scholar
Chakraborti, M. K. 1980. On the pyroclastic rocks of Dalma volcanic sequence, Singhbhum, Bihar. Indian Jl Earth Sci. 7, 216–22.Google Scholar
De, A. 1964. Precambrian Dalma Dhanjori volcanicity of E. India and its stratigraphic significance. Proc. Int. Geol. Cong. 10, 5970.Google Scholar
Dunn, J. A. 1929. The geology of north Singhbhum including parts of Ranchi and Manbhum dists. Mem. Geol. Surv. India 54, 166.Google Scholar
Dunn, J. A. & Dey, A. K. 1942. The geology and petrology of E. Singhbhum and surrounding areas. Mem. Geol. Surv. India 69 (2), 281456.Google Scholar
Fisher, R. V. 1971. Features of coarse grained high concentration fluids and their deposits. J. sedim. Petrol. 41 (4), 916–27.Google Scholar
Gelinas, L., Lajoie, J. & Brooks, C. 1977. The origin and significance of Archaean ultramafic volcaniclastics from Spinifex Ridge, Lamotte Township. Spec. Pap. Quebec Geol. Assn. Canada 16, 297309.Google Scholar
Green, D. H., Nicholls, I. A., Viljoen, M. & Viljoen, R. 1975. Experimentaldemonstration of the existence of peridotitic liquids in earliest Archaean magmatism. Geology 3, 1114.Google Scholar
Gupta, A. & Basu, A. 1979. On the occurrence of pillow lavas in Dalma metavolcanics, Singhbhum, Bihar. J. geol. Soc. India 20, 42–4.Google Scholar
Gupta, A., Basu, A. & Ghosh, P. K. 1980. The Proterozoic ultramafic and mafic tuffs and lavas of the Dalma greenstone belt, Singhbhum, Bihar, E. India. Can. J. Earth Sci. 17, 210–31.CrossRefGoogle Scholar
Gupta, A., Basu, A. & Singh, S. K. 1977. On the occurrence of pyroclastic conglomerate in Dalma metavolcanics, Bihar, India. Indian Jl Earth Sci. 4, 160–8.Google Scholar
McCall, G. J. H. 1977. The Archaean. Stroudsburg: Dowden, Hutchinsonand Ross.Google Scholar
Naha, K. & Ghosh, S. K. 1960. Archaean palaeogeography of E. and N. Singhbhum. Geol. Mag. 97, 436–9.CrossRefGoogle Scholar
Pearce, T. H. & Birkett, T. C. 1974. Archaean metavolcanic rocks from Thackerrsay Township, Canada. Can. Mineralogist 12, 509.Google Scholar
Sarkar, S. N. & Saha, A. K. 1977. The present status of the Precambrian stratigraphy, tectonics and geochronology of Singhbhum-Keonjhar-Mayurbhanj region, E. India. Indian Jl Earth Sci. S. Ray Vol., 3765.Google Scholar
Shapiro, L. & Brannock, W. W. 1955. Rapid analysis of silicate, carbonate and phosphate rocks. Bull. U.S. geol. Surv. 11444.Google Scholar
Viljoen, R. P. & Viljoen, M. J. 1969. Evidence for the composition of the primitive mantle and its products of partial melting from a study of the mafic and ultramafic rocks of the Barberton Mountainland. Spec. Pub. geol. Soc. S. Africa 2, 275–95.Google Scholar