Magnetic anisotropy produced by magma flow: theoretical model and experimental data from Ferrar dolerite sills (Antarctica)
Volcanic rocks forming sills, dykes or lava flows may display a magnetic anisotropy derived from the viscous flow during their emplacement. We model a sill as a steady-state flow of a Bingham fluid, driven by a pressure gradient in a horizontal conduit. The magma velocity as a function of depth is c...
Published in: | Geophysical Journal International |
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Main Authors: | , , |
Format: | Text |
Language: | English |
Published: |
Oxford University Press
1997
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Subjects: | |
Online Access: | http://gji.oxfordjournals.org/cgi/content/short/128/1/230 https://doi.org/10.1111/j.1365-246X.1997.tb04083.x |