Glacial and Glacial and Glaciomarine Sedimentation: Halibut Channel, Grand Banks of Newfoundland | springerprofessional.de

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1997 | OriginalPaper | Buchkapitel

Glacial and Glacial and Glaciomarine Sedimentation: Halibut Channel, Grand Banks of Newfoundland

verfasst von : K. Moran, G. B. J. Fader

Erschienen in: Glaciated Continental Margins

Verlag: Springer Netherlands

Enthalten in: Professional Book Archive

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The Grand Banks of Newfoundland primarily consists of thin (<20 m) Holocene surficial sediments overlying well-indurated Cretaceous and Tertiary bedrock. Glaciomarine sediments are generally absent, however, Halibut Channel, on the Central Grand Banks (Fig. 1) provides a unique window of Pleistocene sediments.

Titel: Glacial and Glacial and Glaciomarine Sedimentation: Halibut Channel, Grand Banks of Newfoundland
verfasst von: K. Moran
G. B. J. Fader
Verlag: Springer Netherlands
Buch: Glaciated Continental Margins
Print ISBN: 978-0-412-79340-0

Electronic ISBN: 978-94-011-5820-6

Copyright-Jahr: 1997
DOI: https://doi.org/10.1007/978-94-011-5820-6_78