The Sinclair Sequence : U- Pb age constraints from the Awasib Mountain area / B. G. Hoal; L. M. Heaman

By:

Hoal, B. H

Contributor(s):

Heaman, L.M

Material type: Text

TextLanguage: English Series: Communications of the Geological Survey of Namibia, Volume 10, 1995 ; p. 83-91Publication details: Windhoek : Geological Survey of Namibia, 1995,: Multi ServicesDescription: 9 pages : tables, fig; 30 cmISSN:

0256-1697

Subject(s):

DDC classification:

PER 553 Communications of the Geological Survey of Namibia

Summary: 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

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Books	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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