The Sinclair Sequence : U- Pb age constraints from the Awasib Mountain area / B. G. Hoal; L. M. Heaman
Material type:![Text](/opac-tmpl/lib/famfamfam/BK.png)
- 0256-1697
- PER 553 Communications of the Geological Survey of Namibia
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Namibia Scientific Society Library | Not for loan |
Special issue: Proterozoic crustal and metallogenic evolution References
The Sinclair Sequence comprises a volcano-sedimentary succession with associated high-level granitoids which is situated adjacent to the Grenville-age Namaqualand Metamorphic Complex in the southern part of Namibia. It forms part of a curvilinear outcrop of Mid- Proterozoic rocks that extends along the southwestern and northwestern margins of the Namibia Province. The geotectonic setting of this association has been interpreted as an ancient active continental margin, an aulacogen, an intracontinetal rift and a collision-related rift
Geological Survey of Namibia Serie
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