U-Pb ages in zircon of the Grão Mogol diamond-bearing conglomerate (Espinhaço Supergroup): implications for the diamond origin in the Espinhaço Range in Minas Gerais.
The
Espinhaço Range in the Grão Mogol region, center-north of Minas Gerais
state, is composed by fine grained quartzites with large cross
stratifications (Resplandecente Formation), which are covered with
erosional unconformity by monomictic conglomerates, and medium to coarse
grained quartzites (Grão Mogol Formation), both units belonging to the
Espinhaço Supergroup, of Proterozoic age. At the locality known as
"Pedra Rica" (signify Rich Rock, an old diamond digging), rocks of these
formations were sampled and separated detrital zircons to acquire U-Pb
by Laser Ablation Inductively LA-ICPMS) ages. The analyzed grains are
rounded to slightly rounded and show oscillatory zoning. The obtained
results indicate a maximum depositional age of 1,595 ± 20 Ma for the
Resplandecente Formation, and 1,052 ± 50 Ma for the Grão Mogol
Formation. The comparison between the obtained data and the available
ages for the Diamantina region and proximities, in the same diamond
province, indicates a strong evidence for the existence of at least two
primary mineralizing events in the basin, in the age range of 1.35 to
1.05 Ga.
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