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...

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Bibliographic Details
Published in:Geophysical Journal International
Main Authors: Dragoni, Michele, Lanza, Roberto, Tallarico, Andrea
Format: Text
Language:English
Published: Oxford University Press 1997
Subjects:
Online Access:http://gji.oxfordjournals.org/cgi/content/short/128/1/230
https://doi.org/10.1111/j.1365-246X.1997.tb04083.x