Figure F2. Seismic profile across the continental slope–rise of the Newfoundland rifted margin showing the location of Site 1277 on the Mauzy Ridge, a high located directly oceanward of magnetic Anomaly M1, inferred to be Early Cretaceous (late Barremian) in age (from Tucholke and Sibuet this volume).

Figure F2. Seismic profile across the continental slope–rise of the Newfoundland rifted margin showing the location of Site 1277 on the Mauzy Ridge, a high located directly oceanward of magnetic Anomaly M1, inferred to be Early Cretaceous (late Barremian) in age (from Tucholke and Sibuet this volume).