Titlebook: Recent Advances in Rock Magnetism, Environmental Magnetism and Paleomagnetism; International Confer Danis Nurgaliev,Valery Shcherbakov,Simo

構(gòu)想

Evidence for the Existence of the Gothenburg and Mono Lake Excursions Based on Paleomagnetic Data fr of the core was radiocarbon dated to 29 ka BP. The paleomagnetic record from the sediments of Baunt Lake reveals and documents for the first time the Gothenburg?and Mono-Lake magnetic excursions for the lakes of the Baikal region. The high sedimentation rate and a reliable age model permit assessme

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擁護(hù)

Influence of Magnetostatic Interaction on Magnetic Characteristics of Decay Products of Nanodisperses of remanent magnetization of the decay products of the titanomagnetite nanoparticle system is carried out. It is established that the magnetic interactions between nanoparticles with an effective field of less than the coercive field leads to an insignificant decrease in the temperature dependence

縫紉

An Estimate of the Remanent Magnetization in the Case of a Ferromagnet Transformation Accompanied byin the Curie point is estimated. The case is considered when the initial Curie temperature is lower than the temperature at which the structure of the ferromagnet changes. The investigation was carried out on an Ising model in the framework of random interaction fields method.

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Magnetic Properties of Soils from the Volga-Kama Forest-Steppe profile samples of virgin dark-gray forest light loamy soil developed on a Permian (Kazanian stage) siltstone and virgin leached medium-thick fat light-loam chernozem developed on the Quaternary deluvial loam were used. Both soils are characterized by accumulative type of magnetic susceptibility an

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Magnetic Properties of Artificial CRM Created on Titanomagnetite-Bearing Oceanic BasaltsM) with .?≈?200?°C was carried out by annealing at different temperatures . for different time intervals up to 200-hour exposure in the external field .?=?50?μT. Monitoring the CRM value against annealing time revealed a strong correlation between the CRM intensity and a strong field magnetization .