The continental shelf
作者:
C. A. Cotton,
期刊:
New Zealand Journal of Geology and Geophysics
(Taylor Available online 1966)
卷期:
Volume 9,
issue 1-2
页码: 105-110
ISSN:0028-8306
年代: 1966
DOI:10.1080/00288306.1966.10420199
出版商: Taylor & Francis Group
数据来源: Taylor
摘要:
Explorations of the structure of the piles of sediment underlying parts of the continental shelf, or terrace, have confirm the theory that in general this ubiquitous feature has been formed by up- and out-growth due to the deposition on the shelf (as topsets beds) and on the continental slope (as foreset beds) during a prolonged movement of either continous or intermittent submergence.
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