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Fig. 6 | Earth, Planets and Space

Fig. 6

From: A comprehensive paleomagnetic study from the last Plinian eruptions of Popocatepetl volcano: absolute chronology of lavas and estimation of emplacement temperatures of PDCs

Fig. 6

Variation 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 intensity

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