Fig. 6From: A comprehensive paleomagnetic study from the last Plinian eruptions of Popocatepetl volcano: absolute chronology of lavas and estimation of emplacement temperatures of PDCsVariation of the NRM intensity and magnetic susceptibility for the three studied lavas and scoria clast, together with lines of constant ratio (Q = NRM/κ·H); the ratio between remanent and induced magnetizations, where κ is the initial magnetic susceptibility and H = 33 Am−1 the magnetic field intensityBack to article page