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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National Institute of Polar Research
1964
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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 |
_version_ |
1766366930284838912 |