Precambrian of the African Continent

P(論文) Precambrian rocks are exclusively found in the vast shield areas such as the Antarctic and the African Continents. Drastic revision of Precambrian geology in the African Continent has been done in recent years. Current knowledge on Craton and Precambrian orogenic belt, on relationship among Pr...

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Main Author: Suwa, Kanenori
Language:English
Published: 1979
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/1024/files/KJ00000011568.pdf
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spelling ftnipr:oai:nipr.repo.nii.ac.jp:00001024 2024-09-09T19:08:54+00:00 Precambrian of the African Continent Suwa, Kanenori 1979-10 application/pdf https://nipr.repo.nii.ac.jp/record/1024/files/KJ00000011568.pdf eng eng Memoirs of National Institute of Polar Research. Special issue 14 93 105 AA00733561 https://nipr.repo.nii.ac.jp/record/1024/files/KJ00000011568.pdf 1979 ftnipr 2024-06-17T04:00:22Z P(論文) Precambrian rocks are exclusively found in the vast shield areas such as the Antarctic and the African Continents. Drastic revision of Precambrian geology in the African Continent has been done in recent years. Current knowledge on Craton and Precambrian orogenic belt, on relationship among Precambrian orogenic belt, continental drift and rift valley, and on two distinct types of structural-metallogenic domains is reviewed in Introduction. The Association for African Studies, Nagoya University made a start in 1962. Some contributions by the Association to Precambrian studies in Africa have been described : Precambrian anorthosites, chromian phlogopite in Bushveld anorthosite, contact aureole of the Bushveld Complex, palaeomagnetism of Precambrian kimberlites, isotope geochemistry of Precambrian carbonatites, geochronology of the Mozambiquian orogenic belt, and metamorphic and plutonic rocks in the Mozambiquian belt around Machakos, Mgama ridge, Linthipe, Aswan and other areas. departmental bulletin paper Other/Unknown Material Antarc* Antarctic Memoirs of National Institute of Polar Research Polar Research National Institute of Polar Research Repository, Japan Antarctic The Antarctic
institution Open Polar
collection National Institute of Polar Research Repository, Japan
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description P(論文) Precambrian rocks are exclusively found in the vast shield areas such as the Antarctic and the African Continents. Drastic revision of Precambrian geology in the African Continent has been done in recent years. Current knowledge on Craton and Precambrian orogenic belt, on relationship among Precambrian orogenic belt, continental drift and rift valley, and on two distinct types of structural-metallogenic domains is reviewed in Introduction. The Association for African Studies, Nagoya University made a start in 1962. Some contributions by the Association to Precambrian studies in Africa have been described : Precambrian anorthosites, chromian phlogopite in Bushveld anorthosite, contact aureole of the Bushveld Complex, palaeomagnetism of Precambrian kimberlites, isotope geochemistry of Precambrian carbonatites, geochronology of the Mozambiquian orogenic belt, and metamorphic and plutonic rocks in the Mozambiquian belt around Machakos, Mgama ridge, Linthipe, Aswan and other areas. departmental bulletin paper
author Suwa, Kanenori
spellingShingle Suwa, Kanenori
Precambrian of the African Continent
author_facet Suwa, Kanenori
author_sort Suwa, Kanenori
title Precambrian of the African Continent
title_short Precambrian of the African Continent
title_full Precambrian of the African Continent
title_fullStr Precambrian of the African Continent
title_full_unstemmed Precambrian of the African Continent
title_sort precambrian of the african continent
publishDate 1979
url https://nipr.repo.nii.ac.jp/record/1024/files/KJ00000011568.pdf
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
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Antarctic
Memoirs of National Institute of Polar Research
Polar Research
genre_facet Antarc*
Antarctic
Memoirs of National Institute of Polar Research
Polar Research
op_relation Memoirs of National Institute of Polar Research. Special issue
14
93
105
AA00733561
https://nipr.repo.nii.ac.jp/record/1024/files/KJ00000011568.pdf
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