Oriented Magnetite Inclusions in Plagioclase: Implications for the Anisotropy of Magnetic Remanence

Abstract Micron to sub‐micron sized ferromagnetic inclusions in rock forming silicate minerals may give rise to particularly stable remanent magnetizations. When a population of inclusions have a preferred crystallographic or shape orientation in a rock, the recorded paleomagnetic direction and inte...

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Hlavní autoři:	O. Ageeva, G. Habler, S. A. Gilder, R. Schuster, A. Pertsev, O. Pilipenko, G. Bian, R. Abart
Médium:	Artigo
Jazyk:	Inglês
Vydáno:	Wiley 2022-02-01
Edice:	Geochemistry, Geophysics, Geosystems
Témata:	plagioclase hosted magnetite micro‐inclusions shape and crystal orientation relationships magnetic fabric anisotropy of magnetic remanence
On-line přístup:	https://doi.org/10.1029/2021GC010272
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