Abstract
Palaeomagnetic samples were collected from 2 dykes belonging to the Gannakouriep dyke swarm, one located in the centre of the Richtersveld subprovince (8215), the other further S in the Steinkopf Domain (8212), where it has been clearly overprinted by a later metamorphic episode. Detailed thermal and A.F. demagnetization indicate that the primary remanence has been extensively overprinted in both dykes. The 40Ar/39Ar step-heating analyses of a whole-rock sample of the 8212 yield a plateau spectrum with an integrated age of 542 + or - 4 Ma; whereas, the 40Ar/39Ar spectrum for a whole-rock sample of 8215 yields a saddle-shaped spectrum with the minimum at approx 400 Ma.-from Authors
| Original language | English (US) |
|---|---|
| Pages (from-to) | 171-183 |
| Number of pages | 13 |
| Journal | Transactions - Geological Society of South Africa |
| Volume | 89 |
| Issue number | 2 |
| State | Published - 1986 |
All Science Journal Classification (ASJC) codes
- General Environmental Science
- General Engineering
- General Earth and Planetary Sciences
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