Thermochronometry and palaeomagnetism of the Archaean Nelshoogte Pluton, South Africa

Abstract

SUMMARY 207Pb/206Pb single-grain zircon, 40Ar/39Ar single-grain hornblende and biotite, and 40Ar/39Ar bulk-sample muscovite and biotite ages from the Nelshoogte trondhjemite pluton located in eastern Transvaal, South Africa, show that this granitoid had a protracted thermal history spanning 3213±4 Ma to about 3000 Ma. Whole-rock 40Ar/39Ar ages from cross-cutting dolerite dykes indicate that these were intruded at about 1900 Ma. There is no evidence of this or other, later events significantly aVecting the argon systematics of the minerals from the pluton dated by the 40Ar/39Ar method. The pluton has a well-defined palaeomagnetic pole which is dated at 3179±18 (2s) Ma by 40Ar/39Ar dating of hornblende. This pole (18°N, 310°E, A 95 =9°) yields a palaeolatitude of 0°, significantly diVerent from other Archaean poles from the Kaapvaal Craton. The palaeolatitude diVerence implies that there was significant apparent polar wander during the Archaean. A second, overprinting magnetization seen in the pluton is also seen in the lower-Proterozoic dolerite dykes, and is consistent with other lower-Proterozoic (2150‐1950 Ma) poles for southern Africa.