Magnetic anisotropy produced by magma flow: theoretical model and experimental data from Ferrar dolerite sills (Antarctica)

Details Magnetic anisotropy produced by magma flow: theoretical model and experimental data from Ferrar dolerite sills (Antarctica) Magnetic anisotropy produced by magma flow: theoretical model and experimental data from Ferrar dolerite sills (Antarctica)

Jan 1997

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1997geoji.128..230d&link_type=ejournal

Geophysical Journal International, vol. 128, issue 1, pp. 230-240

Physics

13

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