TY - JOUR
T1 - Laser ablation ICP mass spectrometry for zircon U-Pb geochronology of metamorphosed granite from the Salem Block
T2 - Implication for Neoarchean crustal evolution in southern India
AU - Sato, Kei
AU - Santosh, M.
AU - Tsunogae, Toshiaki
AU - Chetty, T. R.K.
AU - Hirata, Takafumi
PY - 2011
Y1 - 2011
N2 - We 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 of 207Pb/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.
AB - We 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 of 207Pb/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.
KW - Granulite facies metamorphism
KW - Laser ablation ICP mass spectrometry (LA-ICP-MS)
KW - Salem Block
KW - Southern Granulite Terrane in India
KW - Zircon geochronology
UR - http://www.scopus.com/inward/record.url?scp=79952594954&partnerID=8YFLogxK
U2 - 10.2465/jmps.091222
DO - 10.2465/jmps.091222
M3 - Article
SN - 1345-6296
VL - 106
SP - 1
EP - 12
JO - Journal of Mineralogical and Petrological Sciences
JF - Journal of Mineralogical and Petrological Sciences
IS - 1
ER -