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Magnetic anomalies observed in the zero-field cooled magnetization curves at low temperatures may be related to an appearance of magnetic moment at the Cu ion site.
Electrons and ions over magnetic anomalies observed at ~100 km altitude.
Fig. 3. Electrons and ions over magnetic anomalies observed at ~25 km altitude.
The magnetic anomalies observed in the study area were assumed to have resulted from the basement as well as magnetic materials contained within the fractured/faulted zones relative to the fresh massive bedrock.
LMAG measured the vector magnetic field with a sampling frequency of 32 Hz and a resolution of 0.1 nT. Figure 1 shows an example of the electrons and ions over magnetic anomalies observed at ~100 km altitude.
The study in the area surrounding the Rybnik urban agglomeration (southern Poland) was conducted to determine the influence of various emission sources on the occurrence of local magnetic anomalies observed in the forest topsoils.
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The electron acceleration and ion deceleration over the magnetic anomalies were observed for almost all the encounters with magnetic anomalies at ~25 km altitude.
However, five well-defined positive magnetic anomalies are observed in a line extending southwest from the southern end of Igyo-Sone Bank (M1 to M5 in Figure 3a).
The compound orders ferrimagnetically at TC ≈ 88 K, and at lower temperatures (46 and 10 K), two other magnetic anomalies were observed, probably due to spin reorientations.
The maps of surface distribution of κ value revealed that magnetic anomalies were observed 2.0 km around the residential areas dominated by low emission sources, 2.1 km around the coke plant, 2.8 km around the old steelworks, 1.4 km around the coal-mining waste heaps, and 4.0 km around the combined heat and power plant and coal mines.
The signature of a magnetic anomaly was observed by magnetometer at 0750 UT when Kaguya was at −26.4 deg.
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magnetic events observed
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magnetic polarities observed
magnetic ripples observed
magnetic effects observed
magnetic fluctuations observed
magnetic anomalies evident
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