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- W2004134301 startingPage "3013" @default.
- W2004134301 abstract "Continuous seismic profiles supplemented by soundings and bottom samples were used to discern the structural framework of the Gulf of Maine, a rectangular depression off New England. The central section of the gulf consists of pre-Triassic igneous and metamorphic rocks and Jurassic igneous rocks covered by a thin veneer of Pleistocene and Recent sediments. The Acadian Triassic basin extends 120 km beyond the mouth of the Bay of Fundy into the Gulf of Maine. No definite evidence of a marginal fault was found along the north-west edge of the basin. Cretaceous and Tertiary sediments occur only near Georges Bank and in the area of Cape Cod Bay; in the past these deposits probably extended throughout the gulf. The Gulf of Maine is believed to have been formed by preglacial fluvial erosion and by glacial erosion." @default.
- W2004134301 created "2016-06-24" @default.
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- W2004134301 date "1966-06-15" @default.
- W2004134301 modified "2023-09-23" @default.
- W2004134301 title "Structural framework of the Gulf of Maine" @default.
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- W2004134301 doi "https://doi.org/10.1029/jz071i012p03013" @default.
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