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Because of a connection between activity within the parahippocampus and naturally-occurring geomagnetic activity established in a previous publication [10] and its prominent role as an integrator of experience before long-term memory processes within the hippocampus, inferences of left and right parahippocampal current source density (μA·mm-2) were computed in sLORETA [21] within the classical frequency bands used in more conventional electroencephalographic studies [i.e. delta (1.5–4 Hz); theta (4–7 Hz); low-alpha (7–10 Hz); high-alpha (10–13 Hz); beta-1 (13–20 Hz); beta-2 (20–25 Hz); beta-3 (25–30 Hz); gamma (>30 Hz)].
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