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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Main Author: Takahiro SATO
Format: Article
Language:English
Published: National Institute of Polar Research 1964-03-01
Series:Antarctic Record
Online Access:https://doi.org/10.15094/00007332
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spelling doaj-4d102c2ea8dd485d9170102cc8604d1c2020-11-25T00:05:02ZengNational Institute of Polar ResearchAntarctic Record0085-72892432-079X1964-03-01211777178710.15094/00007332Submarine Topography and Several Bottom Sediments around Prince Olav and Prince Harald Coasts, AntarcticaTakahiro SATO0The Hydrographic OfficeThe 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.https://doi.org/10.15094/00007332
collection DOAJ
language English
format Article
sources DOAJ
author Takahiro SATO
spellingShingle Takahiro SATO
Submarine Topography and Several Bottom Sediments around Prince Olav and Prince Harald Coasts, Antarctica
Antarctic Record
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
series Antarctic Record
issn 0085-7289
2432-079X
publishDate 1964-03-01
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.
url https://doi.org/10.15094/00007332
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