B. Seth et al., Archaean to Neoproterozoic magmatic events in the Kaoko belt of NW Namibiaand their geodynamic significance, PRECAMB RES, 92(4), 1998, pp. 341-363
Age relationships in the N-S trending Neoproterozoic (Pan-African) Kaoko be
lt of northwestern Namibia are still poorly constrained. U-Pb and Pb-Pb zir
con age determinations by single grain evaporation, conventional multigrain
fraction analyses and ion microprobe (SHRIMP) from a profile along the E-W
Hoanib River reveal various episodes of zircon growth, ranging from late A
rchaean to late Neoproterozoic. From the eastern part of the profile we rep
ort crystallization ages of gneiss protoliths from 2645 to 2585 Ma, the old
est ages so far found in Namibia. Sm-Nd isotope data suggest the involvemen
t of still older crustal material in the generation of these gneisses.
A thermal event at ca 2285 Ma ago caused new zircon growth in the Archaean
rocks, and major igneous activity between 1985 and 1960 Ma is represented b
y granitoid intrusions. This demonstrates that these gneisses were part of
the Congo craton since Palaeoproterozoic times. An emplacement age of ca 15
00 Ma was determined for the protolith of a granitic orthogneiss within the
central part of the Hoanib River profile. This is the first record of a ma
gmatic event of this age in this region.
The western part of the profile consists of granitoid rocks that were gener
ated during the Neoproterozoic Damara orogeny. This terrain has previously
been interpreted as a Neoproterozoic metasedimentary domain and subsequentl
y as pre-Damaran basement, but our study proves these rocks to be igneous i
n origin with emplacement ages ranging from 552 to 656 Ma. Sm-Nd isotope da
ta and zircon xenocrysts demonstrate the involvement of older crustal mater
ial in the generation of these granitoids. We interpret a coastal granite,
dated at ca 564 Ma, as being emplaced during the last peak of high-grade me
tamorphism in the Kaoko belt, which is approximately synchronous with the l
ast metamorphic event in the Damara belt of central Namibia. (C) 1998 Elsev
ier Science B.V. Al rights reserved.