SUBSIDENCE OF ATLANTIC-TYPE CONTINENTAL-MARGIN OFF NEW-YORK

The continental margin off New York consists of a thick sequence of at least 4.8 km of mainly shallow-water sediments. Such large thicknesses of shallow-water sediments cannot be produced by the effects of sediment loading alone. We have used biostratigraphic data from the COST B-2 well to examine t...

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Detalhes bibliográficos
Principais autores: Steckler, M, Watts, A
Formato: Journal article
Idioma:English
Publicado em: 1978