U- Pb and Pb- Pb ages of the Naauwpoort rhyolite, Kawakeup leptite and Okongava Diorite: : implications for the onset of rifting and of orogenesis in the Damara belt, Namibia / G. S. de Kock; B. Eglington; R. A. Armstrong; R. E. Harmer; F. Walraven.

By:

de Kock, G. S

Contributor(s):

Eglington, B.Armstrong, R.A.Harmer, R.E.Walraven, F

Material type: Text

TextLanguage: English Series: Communications of the Geological Survey of Namibia special Commemorative issue. P.81-88 Map; sketches; ill. table; graphs; ; Vol.12Publication details: Windhoek : Nam Print, 2002Description: P.8 : map, illustrations, sketches, graph, table; 30 cmSubject(s):

DDC classification:

PER 553 Communications of the Geological Survey of Namibia

Summary: The Naauwpoort quartz porphyry formed during local synsedimentary volcanism towards the end of the initial rifting phase in the central Damara belt of Namibia. The Pan African belts of Namibia consist of the north-south trending Gariep and Kaoko belts and the northeast trending, intracontinental Damara belt.

Tags from this library: No tags from this library for this title.

Average rating: 0.0 (0 votes)

Holdings
Item type	Current library	Call number	Status	Date due	Barcode
Books	Namibia Scientific Society Library		Not for loan

References on page 88.

The Naauwpoort quartz porphyry formed during local synsedimentary volcanism towards the end of the initial rifting phase in the central Damara belt of Namibia. The Pan African belts of Namibia consist of the north-south trending Gariep and Kaoko belts and the northeast trending, intracontinental Damara belt.

Serie

There are no comments on this title.

to post a comment.