P. Wasilewski et G. Kletetschka, Lodestone: Natures only permanent magnet - What it is and how it gets charged, GEOPHYS R L, 26(15), 1999, pp. 2275-2278
Magnetite and Titanomagnetite exhibit magnetic properties which are attribu
table to the micro-structures developed during oxidation and exsolution: Al
l magnetite iron ores which are lodestones contain maghemite. These lodesto
nes have He between 10 and 30 mT, SIRM between 8 and 18 Am(2)kg(1), and R-1
between 0.10 and 0.26. Magnetite, titanomagnetite and metals have REM valu
es (ratio of NRM to SWM) < 0.05. Samples (called fulgarites) obtained from
the Smithsonian Institution have REM values ranging from 0.45 to 0.92. The
REM value serves as a witness parameter to the magnetic fields associated w
ith the lightning bolt. If a high REM value (say >> 0.1) can be verified as
not to be due to contamination by man and does not contain MD hematite the
n the rock has LRM (lightning remanent magnetization). The magnetic field a
ssociated with lightning can be revealed from an isothermal remanent acquis
ition (RA) curve.