Title: Fossil Deep-Sea Channel on the Aleutian Abyssal Plain
Abstract: The discovery of a leveed deep-sea channel whose axial gradient reverses near the Aleutian trench supports the hypothesis that the downbowing of the trench interrupted the turbidity current processes that constructed the Aleutian abyssal plain.
Publication Year: 1969
Publication Date: 1969-01-24
Language: en
Type: article
Indexed In: ['crossref', 'pubmed']
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Cited By Count: 9
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