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- W1597476578 abstract "ABSTRACT New bathymetry, gravity and Pliocene - Quaternary sediment isopach maps have been compiled and gridded for the Scotian margin. A large positive gravity anomaly exists over the Laurentian Fan, which is the major Pliocene - Quaternary depocentre on the Scotian margin. This gravity anomaly is not related to deep structure but can be largely explained by considering the Pliocene-Quaternary sediments as isostatically uncompensated. This implies that the underlying continental margin lithosphère has had considerable strength for at least 3 Ma. Some residual anomalies not accounted for by Pliocene-Quaternary sediment thickness may represent thicker Miocene depocentres, but improved seismic and stratigraphie data are required to assess this possibility. The technique of gravity identification of major sediment depocentres is a useful reconnaissance tool in certain circumstances, such as where there is a topographic expression and the deposit is thick and of major areal extent." @default.
- W1597476578 created "2016-06-24" @default.
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- W1597476578 date "2007-11-29" @default.
- W1597476578 modified "2023-10-03" @default.
- W1597476578 title "The Gravity Signature of a Large Quaternary Depocentre off Southeastern Canada" @default.
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- W1597476578 doi "https://doi.org/10.7202/032919ar" @default.
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