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...
Published in: | Geophysical Journal International |
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Main Authors: | , , , |
Format: | Text |
Language: | English |
Published: |
Oxford University Press
2011
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Subjects: | |
Online Access: | http://gji.oxfordjournals.org/cgi/content/short/186/1/155 https://doi.org/10.1111/j.1365-246X.2011.05029.x |