Study of the nickel silicates associated with the ultrabasic rocks of Nuggihalli schist belt, mysore state

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Naganna, C. and Phene, S.G. (1968) Study of the nickel silicates associated with the ultrabasic rocks of Nuggihalli schist belt, mysore state. Proceedings: Plant Sciences, 67 (4). pp. 174-179. ISSN 0370-0097

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Official URL: http://link.springer.com/article/10.1007%2FBF03053...

Abstract

The occurrence of some nickel silicate minerals as encrustations along joint planes and shear zones of the chromite bearing ultrabasic rocks of Nuggihalli schist belt is described. Chemical and X-ray study shows besides amorphous nickel silicate, the presence of granierite, nepouite or nickel antigorite. The nickel minerals are secondary developed by the action of circulating waters. The source of nickel is olivine, in the structure of which Ni is known to be present, either as camouflaged or captured ion.

Item Type: Article
Subjects: Faculty of Science > Earth Sciences > Geology
Divisions: Jnana Bharathi / Central College Campus > Department of Geology
Depositing User: Mr. Ramaprasad C
Date Deposited: 29 Aug 2016 06:15
Last Modified: 29 Aug 2016 06:15
URI: http://eprints-bangaloreuniversity.in/id/eprint/4912

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