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Laser ablation ICP mass spectrometry for zircon U-Pb geochronology of metamorphosed granite from the Salem Block: Implication for Neoarchean crustal evolution in southern India

dc.contributor.authorSato, Kei
dc.contributor.authorSantosh, M.
dc.contributor.authorTsunogae, T
dc.contributor.authorChetty, T.R.K.
dc.contributor.authorHirata, Takafumi
dc.date.accessioned2015-12-10T22:27:48Z
dc.date.issued2011
dc.date.updated2016-02-24T09:04:36Z
dc.description.abstractWe report here petrological characteristics of metamorphosed granite and metagabbro from the Kanja Malai hills, the southern margin of the Salem Block in southern India. Field observations suggest that both these rock types experienced high-grade metamorphism, and exhibit strong foliation. Many of cores of zircons extracted from the granite show an internal structure suggesting magmatic crystallization. In contrast, rims of the zircons commonly display metamorphic overgrowth. We also present geochronological data utilizing laser ablation ICP mass spectrometry technique on the zircons that show the weighted means of207Pb/206Pb age of 2647 ± 11 Ma (error: 1σ) for the timing of magmatism, and 2442 ± 20 Ma (error: 1σ) for the subsequent high-grade metamorphism. Together with a previous geochronological study on charnockites from the Salem Block, our results also provide an important constraint on the Neoarchean magmatism (2.65-2.53 Ga) in southern India, correlating the magmatism with a major global crust formation event during the Neoarchean.
dc.identifier.issn1349-3825
dc.identifier.urihttp://hdl.handle.net/1885/54367
dc.publisherJapanese Association of Mineralogists Petrologists and Economic Geologists
dc.sourceJournal of Mineralogical and Petrological Sciences
dc.subjectKeywords: Granulite facies metamorphism; Laser ablation ICP mass spectrometry (LA-ICP-MS); Salem Block; Southern Granulite Terrane in India; Zircon geochronology
dc.titleLaser ablation ICP mass spectrometry for zircon U-Pb geochronology of metamorphosed granite from the Salem Block: Implication for Neoarchean crustal evolution in southern India
dc.typeJournal article
local.bibliographicCitation.issue1
local.bibliographicCitation.lastpage12
local.bibliographicCitation.startpage1
local.contributor.affiliationSato, Kei, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationSantosh, M., Koshi UNiversity
local.contributor.affiliationTsunogae, T, University of Tsukuba
local.contributor.affiliationChetty, T.R.K., National Geophysical Research Institute
local.contributor.affiliationHirata, Takafumi, Kyoto University
local.contributor.authoruidSato, Kei, u4913075
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040303 - Geochronology
local.identifier.absseo970104 - Expanding Knowledge in the Earth Sciences
local.identifier.ariespublicationf5625xPUB299
local.identifier.citationvolume106
local.identifier.doi10.2465/jmps.091222
local.identifier.scopusID2-s2.0-79952594954
local.type.statusPublished Version

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