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Aeromagnetic Survey of the Troodos Igneous Massif, Cyprus

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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