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Recent evidence suggests that a portion of the Canary plume travelled northeastwards below the lithosphere of the Atlas Mountains in North Africa towards the Alboran domain and was captured ∼10 Ma ago by the Gibraltar subduction system in the Western Mediterranean. The capture would have been associated with the mantle return flow induced by the west ward retreating slab that would have …
- Tahun Terbit
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Fakultas Keguruan dan Ilmu Pendidikan
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