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The geological and tectonic evolution of the Rapale formations is shaped by various East Pan African Rift events and Grevilian Orogenies, prominently featuring Rapale Gneiss. The study highlights fragile structures like faults and fractures, alongside ductile formations such as Boudins and high-grade metamorphic structures like migmatites. The spatial orientation of these formations varies, with some extending from 179N to 250N, while others reach up to 360N, indicating the complex interplay of known and unidentified geological events in shaping the region's relief.
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Geotectonic evolution of the Rapale Formations, Dinis Fernando Monjane
- Lingua
- Pubblicato
- 2023
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