NEW PROTEROZOIC K-AR AGES FOR SOME KIMBERLITES AND LAMPROITES FROM THE CUDDAPAH BASIN AND DHARWAR CRATON, SOUTH-INDIA - EVIDENCE FOR NONCONTEMPORANEOUS EMPLACEMENT
Nvc. Rao et al., NEW PROTEROZOIC K-AR AGES FOR SOME KIMBERLITES AND LAMPROITES FROM THE CUDDAPAH BASIN AND DHARWAR CRATON, SOUTH-INDIA - EVIDENCE FOR NONCONTEMPORANEOUS EMPLACEMENT, Precambrian research, 79(3-4), 1996, pp. 363-369
We report new K-Ar age determinations carried out on mica separates fr
om kimberlites and lamproites that occur within and adjacent to the in
tra-cratonic Cuddapah basin in southern India. This work includes the
first ages obtained from the Ramannapeta lamproite (at the northeaster
n margin of the Cuddapah basin) and from one of the kimberlites in the
Mahbubnagar district. The Ramannapeta lamproite and the Kotakonda kim
berlite were both emplaced in the Proterozoic and have ages of 1384 +/
- 18 and 1363 +/- 48 Ma, respectively. These dates are similar to the
1350 +/- 52 Ma age obtained here for the Chelima lamproite (within the
Cuddapah basin). The Muligiripalle kimberlite (Pipe 5 of the Anantapu
r district) on the other hand yielded a much lower age of 1153 +/- 17
Ma. Our results demonstrate that the emplacement of the Indian kimberl
ites and lamproites during the Proterozoic did not take place within t
he span of 30 Ma around 1090 Ma as some workers have recently advocate
d, but occurred over a period of > 300 Ma. The Chelima (within the Cud
dapah basin) and Ramannapeta lamproites represent some of the oldest l
amproites world-wide and, together with the Kotakonda kimberlite, they
might constitute a hitherto unrecognised Proterozoic episode of potas
sic magmatism at similar to 1350-1380 Ma.