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basinal |
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| The stratigraphy consists of deformed and metamorphosed basinal sediments that accumulated at the edge of the Neoproterozoic to Paleozoic continental margin. Regional geologic maps show that the anomalous area is underlain by a large in-belt granite stock intruding mafic volcanic and basinal argillic sediments at the western boundary of the Sefwi greenstone belt. 1997, The role of mixing and migration of basinal waters in carbonate mineral mass transport, in Montanez, I. |
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