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在非洲南部,林波波带和巴伯顿山地的构造演化,可用从约3600Ma直到2500Ma一段时间的板块构造活动幕来解释。尽管时间上有联系,但在每一地区活动类型不同。津巴布韦和卡普瓦尔克拉通的构造演化,可能被认为是两个端元类型的结合。林波波活动带是在3570Ma前由于大陆上升崩塌成地堑而形成的。这种上升出现在含有年龄至少为3790Ma的岩石的克拉通中,并且可能源自地幔羽状体(Mantle plu-
In South Africa, the tectonic evolution of the Limpopo Belt and the Barberton Mountains can be explained by the tectonic activity of the tectonic plates from about 3600Ma to 2500Ma. Although time-related, there are different types of activities in each area. The tectonic evolution of Zimbabwe and Kapoor Cratons may be considered as a combination of two endmember types. Limbo activity belt was formed in 3570Ma as the mainland rose and collapsed into a graben. This rise occurs in cratons containing rocks that are at least 3790 Ma in age and may originate from the Mantle plu-