A shallow shelf around Franklin Island in the Ross Sea, Antarctica
作者:
J. W. Brodie,
期刊:
New Zealand Journal of Geology and Geophysics
(Taylor Available online 1959)
卷期:
Volume 2,
issue 1
页码: 108-119
ISSN:0028-8306
年代: 1959
DOI:10.1080/00288306.1959.10431316
出版商: Taylor & Francis Group
数据来源: Taylor
摘要:
A preferred level of marine erosion at a depth of 50 fathoms truncates banks around Franklin Island and forms a shelf similar in form to the continental shelves of temperate regions.
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