Precambrian of the African Continent

K. Suwa
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Abstract

Precambrian rocks are exclusively found in the vast shield areas such as the Antarctic and the African Continents. Drastic revision of Precam­ brian 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, palaeornagnetism of Precambrian kimberlites, isotope geochemistry of Precambrian carbonatites, geochronology of the Mozambiquian orogenic belt, and metamorphic and plu­ tonic rocks in the Mozambiquian belt around Machakos, Mgama ridge, Lin­ thipe, Aswan and other areas.
非洲大陆的前寒武纪
前寒武纪岩石只存在于像南极和非洲大陆这样的巨大盾状地带。近年来,对非洲大陆前脑区地质进行了重大的修正。引言部分对克拉通与前寒武纪造山带、前寒武纪造山带与大陆漂移和裂谷的关系以及两种不同类型的构造成矿域的研究现状进行了综述。名古屋大学非洲研究协会成立于1962年。介绍了协会对非洲前寒武纪研究的一些贡献:前寒武纪斜长岩、Bushveld斜长岩中的铬铁云母、Bushveld杂岩的接触光圈、前寒武纪金伯利岩的古磁性、前寒武纪碳酸盐的同位素地球化学、莫桑比克造山带的年代学以及莫桑比克造山带machaos、Mgama ridge、Lin - thipe、Aswan等地区的变质和富渗岩。
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