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dc.contributor.authorHofmann, A.
dc.contributor.authorMazumder, Rajat
dc.date.accessioned2017-01-30T10:49:58Z
dc.date.available2017-01-30T10:49:58Z
dc.date.created2016-12-01T19:30:21Z
dc.date.issued2015
dc.identifier.citationHofmann, A. and Mazumder, R. 2015. A review of the current status of the Older Metamorphic Group and Older Metamorphic Tonalite Gneiss: insight into the Palaeoarchean history of the Singhbhum craton, India, in Mazumder, R. and Eriksson, P. (ed), Precambrian basins of India: stratigraphic and tectonic contexts, pp. 103-108. London: Geological Society.
dc.identifier.urihttp://hdl.handle.net/20.500.11937/6016
dc.identifier.doi10.1144/M43.7
dc.description.abstract

The Older Metamorphic Group and the Older Metamorphic Tonalite Gneiss are classic examples of Palaeaoarchaean highgrademetamorphic rocks of the Singhbhum Craton of India. The Older Metamorphic Group is a supracrustal assemblage that was probably deposited as a greenstone belt-type succession before c. 3.32 Ga, the low-grade equivalents of which are found in parts of the Iron Ore Group. The Older Metamorphic Tonalite Gneiss represents a suite of granitoids that are tectonically interleaved with the supracrustal gneisses and that formed over an extended period of time, 3.53-3.45 Ga and possibly later, by processes of Archaean crustal growth.

dc.publisherGeological Society
dc.title. A review of the current status of the Older A review of the current status of the Older Metamorphic Group and Older Metamorphic Tonalite Gneiss: insights into the Palaeoarchaean history of the Singhbhum craton, India
dc.typeBook Chapter
dcterms.source.startPage103
dcterms.source.endPage108
dcterms.source.titlePrecambrian basins of India: stratigraphic and tectonic context
dcterms.source.isbn978-1-862397-231
dcterms.source.chapter23
curtin.departmentCurtin Sarawak
curtin.accessStatusFulltext not available


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