Archaean to Neoproterozoic magmatic events in the Kaoko belt of NW Namibiaand their geodynamic significance

Citation
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
Citations number
61
Categorie Soggetti
Earth Sciences
Journal title
PRECAMBRIAN RESEARCH
ISSN journal
03019268 → ACNP
Volume
92
Issue
4
Year of publication
1998
Pages
341 - 363
Database
ISI
SICI code
0301-9268(199812)92:4<341:ATNMEI>2.0.ZU;2-Y
Abstract
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.