Modification of the magnetic mineralogy in basalts due to fluid-rock interactions in a high-temperature geothermal system (Krafla, Iceland)

Active high-temperature (>150 °C) geothermal areas like the Krafla caldera, NE-Iceland, often show distinct magnetic lows in aeromagnetic anomaly maps suggesting a destruction of magnetic minerals by hydrothermal activity. The main alteration processes in such an environment are low-temperature o...

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Bibliographic Details
Published in:Geophysical Journal International
Main Authors: Oliva-Urcia, Belén, Kontny, Agnes, Vahle, Carsten, Schleicher, Anja M.
Format: Text
Language:English
Published: Oxford University Press 2011
Subjects:
Online Access:http://gji.oxfordjournals.org/cgi/content/short/186/1/155
https://doi.org/10.1111/j.1365-246X.2011.05029.x