**ABSTRACT** The study of a garnet‐bearing quartzite from a major suture zone in Iberia reports an unusual high‐T fabric. Quartz __c__‐axis patterns were plotted using shaped garnet as reference axis for the finite stretch (__X__‐axis). The pole figures are characterized by a dominant single maximum
Gravity evidence for a larger Limpopo Belt in southern Africa and geodynamic implications
✍ Scribed by R. T. Ranganai; A. B. Kampunzu; E. A. Atekwana; B. K. Paya; J. G. King; D. I. Koosimile; E. H. Stettler
- Publisher
- John Wiley and Sons
- Year
- 2002
- Tongue
- English
- Weight
- 364 KB
- Volume
- 149
- Category
- Article
- ISSN
- 0956-540X
No coin nor oath required. For personal study only.
📜 SIMILAR VOLUMES
The Rio Magno Unit (RMU) tectonically overlies the Schistes Lustrés units in south‐eastern Alpine Corsica. It is represented by an ophiolitic sequence, showing remarkable differences with respect to the commonly recognized Corsican ophiolites. This unit can be distinguished from the Schistes Lustrés
Structural analyses of Palaeozoic Cape Supergroup outcrops in several areas within the Eastern Cape Fold Belt show that there are a number of thrust sheets hundreds of metres thick cropping out in more or less strike-parallel belts up to 5 km wide. Individual thrusts within the thrust sheets are com