Abstract
Comparison of palaeomagnetic poles from the Guayana Shield with the published Precambrian palaeomagnetic record for Africa suggests that large-scale (thousands of kilometres) transcurrent motions have occurred along Upper Proterozoic mobile belts in South America and Africa. Displacements of such magnitude are consistent with a transform model for Precambrian mobile belts.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 131-136 |
| Number of pages | 6 |
| Journal | Nature |
| Volume | 289 |
| Issue number | 5794 |
| DOIs | |
| State | Published - 1981 |
All Science Journal Classification (ASJC) codes
- General
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