Submarine Topography and Several Bottom Sediments around Prince Olav and Prince Harald Coasts, Antarctica

The deep sea floor between Africa and Antarctica is divided into two provinces by the continuation of Mid-Atlantic Ridge. The bottom sediments on the continental slope around Prince Olav Coast and Amundsen Bay are hemipelagic clays which are rich in SiO_2 and poor in CaCO_3, Fe_2O_3, Al_2O_3 and P_2...

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Bibliographic Details
Main Author: Takahiro SATO
Format: Article in Journal/Newspaper
Language:English
Japanese
Published: National Institute of Polar Research 1964
Subjects:
Online Access:https://doi.org/10.15094/00007332
https://doaj.org/article/4d102c2ea8dd485d9170102cc8604d1c
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spelling ftdoajarticles:oai:doaj.org/article:4d102c2ea8dd485d9170102cc8604d1c 2023-05-15T13:22:47+02:00 Submarine Topography and Several Bottom Sediments around Prince Olav and Prince Harald Coasts, Antarctica Takahiro SATO 1964-03-01T00:00:00Z https://doi.org/10.15094/00007332 https://doaj.org/article/4d102c2ea8dd485d9170102cc8604d1c EN JA eng jpn National Institute of Polar Research https://doi.org/10.15094/00007332 https://doaj.org/toc/0085-7289 https://doaj.org/toc/2432-079X doi:10.15094/00007332 0085-7289 2432-079X https://doaj.org/article/4d102c2ea8dd485d9170102cc8604d1c Antarctic Record, Iss 21, Pp 1777-1787 (1964) Geography (General) G1-922 article 1964 ftdoajarticles https://doi.org/10.15094/00007332 2023-01-08T01:35:23Z The deep sea floor between Africa and Antarctica is divided into two provinces by the continuation of Mid-Atlantic Ridge. The bottom sediments on the continental slope around Prince Olav Coast and Amundsen Bay are hemipelagic clays which are rich in SiO_2 and poor in CaCO_3, Fe_2O_3, Al_2O_3 and P_2O_5. Article in Journal/Newspaper Amundsen Bay Antarc* Antarctica Prince Olav Coast Directory of Open Access Journals: DOAJ Articles Mid-Atlantic Ridge Prince Olav Coast ENVELOPE(41.000,41.000,-69.000,-69.000) Amundsen Bay ENVELOPE(50.000,50.000,-66.917,-66.917)
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
Japanese
topic Geography (General)
G1-922
spellingShingle Geography (General)
G1-922
Takahiro SATO
Submarine Topography and Several Bottom Sediments around Prince Olav and Prince Harald Coasts, Antarctica
topic_facet Geography (General)
G1-922
description The deep sea floor between Africa and Antarctica is divided into two provinces by the continuation of Mid-Atlantic Ridge. The bottom sediments on the continental slope around Prince Olav Coast and Amundsen Bay are hemipelagic clays which are rich in SiO_2 and poor in CaCO_3, Fe_2O_3, Al_2O_3 and P_2O_5.
format Article in Journal/Newspaper
author Takahiro SATO
author_facet Takahiro SATO
author_sort Takahiro SATO
title Submarine Topography and Several Bottom Sediments around Prince Olav and Prince Harald Coasts, Antarctica
title_short Submarine Topography and Several Bottom Sediments around Prince Olav and Prince Harald Coasts, Antarctica
title_full Submarine Topography and Several Bottom Sediments around Prince Olav and Prince Harald Coasts, Antarctica
title_fullStr Submarine Topography and Several Bottom Sediments around Prince Olav and Prince Harald Coasts, Antarctica
title_full_unstemmed Submarine Topography and Several Bottom Sediments around Prince Olav and Prince Harald Coasts, Antarctica
title_sort submarine topography and several bottom sediments around prince olav and prince harald coasts, antarctica
publisher National Institute of Polar Research
publishDate 1964
url https://doi.org/10.15094/00007332
https://doaj.org/article/4d102c2ea8dd485d9170102cc8604d1c
long_lat ENVELOPE(41.000,41.000,-69.000,-69.000)
ENVELOPE(50.000,50.000,-66.917,-66.917)
geographic Mid-Atlantic Ridge
Prince Olav Coast
Amundsen Bay
geographic_facet Mid-Atlantic Ridge
Prince Olav Coast
Amundsen Bay
genre Amundsen Bay
Antarc*
Antarctica
Prince Olav Coast
genre_facet Amundsen Bay
Antarc*
Antarctica
Prince Olav Coast
op_source Antarctic Record, Iss 21, Pp 1777-1787 (1964)
op_relation https://doi.org/10.15094/00007332
https://doaj.org/toc/0085-7289
https://doaj.org/toc/2432-079X
doi:10.15094/00007332
0085-7289
2432-079X
https://doaj.org/article/4d102c2ea8dd485d9170102cc8604d1c
op_doi https://doi.org/10.15094/00007332
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