Abstract
Aeromagnetic data, combined with other observations, support the view that some of the crust beneath the eastern Mediterranean might be oceanic, formed by seafloor spreading at a time when the Earth's magnetic field was of constant and normal polarity.
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VINE, F., POSTER, C. & GASS, I. Aeromagnetic Survey of the Troodos Igneous Massif, Cyprus. Nature Physical Science 244, 34–38 (1973). https://doi.org/10.1038/physci244034a0
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DOI: https://doi.org/10.1038/physci244034a0
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