The timing of ultrahigh-temperature metamorphism in Southern India: U-Th-Pb electron microprobe ages from zircon and monazite in sapphirine-bearing granulites

Copyright © 2006 International Association for Gondwana Research Published by Elsevier B.V.We report here U-Pb electron microprobe ages from zircon and monazite associated with corundum- and sapphirine-bearing granulite facies rocks of Lachmanapatti, Sengal, Sakkarakkottai and Mettanganam in the Palghat-Cauvery shear zone system and Ganguvarpatti in the northern Madurai Block of southern India. Mineral assemblages and petrologic characteristics of granulite facies assemblages in all these localities indicate extreme crustal metamorphism under ultrahigh-temperature (UHT) conditions. Zircon cores from Lachmanapatti range from 3200 to 2300 Ma with a peak at ∼ 2420 Ma, while those from Mettanganam show ∼ 2300 Ma peak. Younger zircons with peak ages of ∼ 2100 and ∼ 830 Ma are displayed by the UHT granulites of Sengal and Ganguvarpatti, although detrital grains with ∼ 2000 Ma ages are also present. The Late Archaean-aged cores are mantled by variable rims of Palaeo- to Mesoproterozoic ages in most cases. Zircon cores from Ganguvarpatti range from 2279 to 749 Ma and are interpreted to reflect multiple age sources. The oldest cores are surrounded by Palaeoproterozoic and Mesoproterozoic rims, and finally mantled by Neoproterozoic overgrowths. In contrast, monazites from these localities define peak ages of between 550 and 520 Ma, with an exception of a peak at ∼ 590 Ma for the Lachmanapatti rocks. The outermost rims of monazite grains show spot ages in the range of 510-450 Ma. While the zircon populations in these rocks suggest multiple sources of Archaean and Palaeoproterozoic age, the monazite data are interpreted to date the timing of ultrahigh-temperature metamorphism in southern India as latest Neoproterozoic to Cambrian in both the Palghat-Cauvery shear zone system and the northern Madurai Block. The data illustrate the extent of Neoproterozoic/Cambrian metamorphism as India joined the Gondwana amalgam at the dawn of the Cambrian. © 2006 International Association for Gondwana Research.M. Santosh, A.S. Collins, I. Tamashiro, S. Koshimoto, Y. Tsutsumi and K. Yokoyamahttp://www.elsevier.com/wps/find/journaldescription.cws_home/706719/description#descriptio