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Summary New investigations carried out onshore Nacala in Mozambique prove the occurrence of Oxfordian to Kimmeridgian marine series. This series overlie an older series (Jurassic?) with a marked angular unconformity. These two units demonstrate the occurrence of a proto Mozambique marine channel West of the Davies Ridge and are in line with the results of the offshore exploration wells and help to improve the seismic interpretation at depth.

Reappraisal of Nacala Jurassic Outcrop (onshore Mozambique): A Key to Understanding Offshore Stratigraphy and Petroleum Systems