Ancient Planetary Magnetic Field Intensity from the LL6 St. Severin

Mathematics – Logic

Scientific paper

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[1521] Geomagnetism And Paleomagnetism / Paleointensity, [1595] Geomagnetism And Paleomagnetism / Planetary Magnetism: All Frequencies And Wavelengths

Scientific paper

Magnetic and mineralogic investigation of Chondrites is useful to decipher the early evolution of the solar system and the formation of planetary objects. The natural remanent magnetization (NRM) of LL6 St. Severin chondrite is extremely stable against the nominal demagnetization. A suite of rock magnetic tests, low-temperature saturation isothermal remanence cycling, microscopic observations, and electron microprobe analyses suggested that NRM of St. Severin is carried by fine-grained Kamacite. Considering its low degree of shock-induced effects, St. Severin may faithfully record the ancient planetary magnetic field. The IZZI paleointensity determination was carried out on several chips of St. Severin. Two specimens yielded successful paleointensity without showing signs of any alteration. Estimated magnetic field intensity from the St. Severin is within an order of magnitude of that of the present-day Earth.

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