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Morphology and seismic stratigraphy of the inner continental shelf off Nova Scotia, Canada: Evidence for a −65 m lowstand between 11,650 and 11,250 C14 yr B.P.

GeophysicsMarine Geology−65 M LowstandEngineeringSeismologyNova ScotiaSeismic StratigraphyContinental TectonicsGeographyGeologyContinental MarginEarth ScienceRegional GeologyContinental ShelfTectonics