2001
DOI: 10.2138/am-2001-11-1213
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Aeromagnetic anomalies, magnetic petrology, and rock magnetism of hemo-ilmenite- and magnetite-rich cumulate rocks from the Sokndal Region, South Rogaland, Norway

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Cited by 91 publications
(94 citation statements)
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“…The magnetic anomaly over this deposit grades westward from a negative remanence-dominated anomaly to a positive induced anomaly, most likely related to an increase in the magnetite/hemo-ilmenite ratio from east to west (McEnroe et al, 2001). There are also Fe-Ti mineralizations that depart somewhat from the classification of McEnroe et al (2001).…”
Section: Magnetic Signatures Of Fe-ti-v-p Depositsmentioning
confidence: 86%
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“…The magnetic anomaly over this deposit grades westward from a negative remanence-dominated anomaly to a positive induced anomaly, most likely related to an increase in the magnetite/hemo-ilmenite ratio from east to west (McEnroe et al, 2001). There are also Fe-Ti mineralizations that depart somewhat from the classification of McEnroe et al (2001).…”
Section: Magnetic Signatures Of Fe-ti-v-p Depositsmentioning
confidence: 86%
“…They produce an induced-current magnetic response parallel to the Earth's present-day magnetic field, giving rise to positive anomalies on aeromagnetic maps. The magnetic properties of these rocks are dominated by magnetite; in particular, the viscous NRM behavior is "more or less as predicted from the common behavior of multi-domain magnetite" (McEnroe et al, 2001). Evolved cumulates from the upper part of the layered series of the Bjerkreim-Sokndal intrusion are typical examples of magnetiterich noritic rocks with homogeneous ilmenite giving rise to induced magnetic highs.…”
Section: Magnetic Signatures Of Fe-ti-v-p Depositsmentioning
confidence: 93%
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