The paleomagnetism of the Turkana lavas
The paleomagnetism of the Turkana lavas
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图尔卡纳熔岩的古地磁学
DOI：
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发表时间：
1966
期刊：
影响因子：
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通讯作者：
A. Mussett
中科院分区：
文献类型：
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作者：
P. Raja;T. Reilly;A. Mussett
本文给出了清理肯尼亚西北部中新世熔岩后获得的磁化方向。由此获得的极点位置，加上东非的类似数据，表明从始新世晚期到近代没有发生重大变化。观测到的方向表明，晚中新世逆转的时代已经发生。
Directions of magnetizations obtained after cleaning the Miocene lavas from northwest Kenya are presented. The pole position thus obtained, together with similar data from eastern Africa, indicates that no significant change has occurred from late Eocene to recent times. Observed directions suggest that a late Miocene reversed epoch has occurred.