2004
DOI: 10.1016/j.oregeorev.2003.08.008
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Characterization of sulfide deposits by airborne magnetic and gamma-ray responses in eastern Finland

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Cited by 48 publications
(19 citation statements)
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“…The latter interpretation was motivated by the attempt to explain the magnetic response of the BMA and the spatial correlation of the SCCB due to a common source. Although serpentinite is a candidate for a magnetic anomalous source, modern electrical conductivity measurements on serpentinite reveal it as a poor electrical conductor (Airo and Loukola-Ruskeeniemi, 2004). Our magnetic modelling studies support the existence of an 100 to 150 km broad and 25 km deep reaching magnetic source, but are not consistent with such narrow conductivity anomalies found in both profiles beneath the centre of the BMA.…”
Section: Discussioncontrasting
confidence: 80%
“…The latter interpretation was motivated by the attempt to explain the magnetic response of the BMA and the spatial correlation of the SCCB due to a common source. Although serpentinite is a candidate for a magnetic anomalous source, modern electrical conductivity measurements on serpentinite reveal it as a poor electrical conductor (Airo and Loukola-Ruskeeniemi, 2004). Our magnetic modelling studies support the existence of an 100 to 150 km broad and 25 km deep reaching magnetic source, but are not consistent with such narrow conductivity anomalies found in both profiles beneath the centre of the BMA.…”
Section: Discussioncontrasting
confidence: 80%
“…Magnetic derivatives have been widely used in studying basement structure in Finland (e.g., Airo, 1999;Airo and Loukola-Ruskeeniemi, 2004;Lipponen and Airo, 2006;.…”
Section: Magnetic Lineamentsmentioning
confidence: 99%
“…Airborne radiometric and magnetic surveys have been used extensively in the mineral exploration industry predominantly for the delineation of mineral deposits [1]. Its application ranges from mineral exploration [2], structure mapping and rock characterization [3].…”
Section: Introductionmentioning
confidence: 99%