We report paleomagnetic results from Mezoproterozoic rocks from the Margate and Mzumbe terranes of the Natal belt, KwaZulu-Natal, South Africa. The Port Edward pluton, a member of the Oribi Gorge Suite, yields a pole position at 7.4Β°S, 327.8Β°E, A 95 = 4.2Β°. The magnetic remanence of these magnetite-
Geology and evolution of the Natal belt, South Africa
β Scribed by S. McCourt; R.A. Armstrong; G.H. Grantham; R.J. Thomas
- Publisher
- Elsevier Science
- Year
- 2006
- Tongue
- English
- Weight
- 945 KB
- Volume
- 46
- Category
- Article
- ISSN
- 1464-343X
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The siliciclastic Ordovician Natal Group, distributed along the east coast of South Africa, is a predominantly fluvial sequence deposited by braided streams. Although the strata are not metamorphosed, they have been strongly affected by deep burial diagenesis that left many burial diagenetic texture
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