Palaeomagnetic evidence for the persistence or recurrence of geomagnetic main field anomalies in the South Atlantic
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文摘

A unique paleomagnetic dataset from Tristan da Cunha in the South Atlantic.

Lava flows Ar/Ar dated as 46 to 90 ka.

Average paleointensity 18±6 μT: weaker than global paleomagnetic average.

Data suggest magnetic anomaly present in the Late Pleistocene in the South Atlantic.

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