Af. Trendall et al., A PRECISE ZIRCON U-PB AGE FOR THE BASE OF THE BIF OF THE MULAINGIRI FORMATION, (BABABUDAN GROUP, DHARWAR SUPERGROUP) OF THE KARNATAKA CRATON, Journal of the Geological Society of India, 50(2), 1997, pp. 161-170
SHRIMP U-Pb analyses of zircon grains from two thin dark shales believ
ed to be syndepositional ashfall tuffs close to the base of the banded
iron-formation (BIF) within the Mulaingiri Formation of the Bababudan
Group (Dharwar Supergroup) of the western Karnataka Craton provide a
precise age for the onset of BIF deposition in the basin. Sample 12001
9C, from the exact base of the BIF, gave an age of 2720 +/- 7 Ma, whil
e sample 120018C, 14.5m above the base, gave an age of 2718 +/- 6 Ma.
The second sample contained younger grains which may have been affecte
d by a late thermal event.