Magma flow in the East Greenland dyke swarm inferred from study of anisotropy of magnetic susceptibility: magmatic growth of a volcanic margin - Archive ouverte HAL
Article Dans Une Revue Geophysical Journal International Année : 2004

Magma flow in the East Greenland dyke swarm inferred from study of anisotropy of magnetic susceptibility: magmatic growth of a volcanic margin

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hal-04617962 , version 1 (20-06-2024)

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Jean-Paul Callot, Laurent Geoffroy. Magma flow in the East Greenland dyke swarm inferred from study of anisotropy of magnetic susceptibility: magmatic growth of a volcanic margin. Geophysical Journal International, 2004, 159, pp.816 - 830. ⟨10.1111/j.1365-246x.2004.02426.x⟩. ⟨hal-04617962⟩

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