On the age and morphology of the reunion event
On the age and morphology of the reunion event
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DOI：
10.1029/2000gl008536
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发表时间：
2000-09
影响因子：
5.2
通讯作者：
A. Baksi;K. Hoffman
中科院分区：
文献类型：
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作者：
A. Baksi;K. Hoffman
数据有关的年龄正常极性团聚“事件”（或subchron），以及它是否是一个分裂的功能，严格审查。留尼汪岛两个层序熔岩的新40 Ar/39 Ar年龄测定，沿着可用的钾氩（K-Ar），40 Ar/39 Ar和天体年代学分析，表明年龄为2.15-2.13 Ma。虽然不能完全排除这种可能性，但目前还没有令人信服的证据支持在7 - 9万年后有一个短暂的正常极性的论点。
Data pertinent to the age of the normal polarity Reunion “Event” (or subchron), and whether it is a split feature, are critically examined. New 40Ar/39Ar age determinations on lavas from two sequences on Reunion Island, along with available potassium‐argon (K‐Ar), 40Ar/39Ar and astrochronological analyses, indicate an age of 2.15–2.13 Ma. Although the possibility cannot be completely ruled out, at present there is no convincing evidence supporting the contention of a short duration of normal polarity some 70–90 kyr later.