FERROMAGNETIC PHASES OF MAGNETITE QUARTZITES ACCORDING TO THERMOMAGNETOMETRY AND FERROMAGNETIC RESONANCE DATA
Abstract
Ferromagnetic phases of magnetite quartzites and changes in the magnetic structure of magnetites of the Kremenchug iron ore district were studied. In addition to magnetites with impurities, at least 4 types of cation-deficient magnetites with Curie points near 300, 350, 400, and 500 °C and inversion temperatures above 700 °C were found in the ores.
In magnetite in association with cumingtonite on DTMA, splitting of the peak of magnetite with TC = 546 into peaks with TC= 517 and 570 oС of approximately the same intensity was detected. It is shown that this phenomenon indicates the presence in the ore of two types of magnetite with TC =502 and 539 oС with greater and lesser coercive force, respectively.

Geological structure and history of the geological development of the Ukrainian shield (to the 100th anniversary of the birth of Academician of the National Academy of Sciences of Ukraine M.P. Shcherbak)
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Pages
157-161
Published
August 15, 2024
Copyright (c) 2024 Press of the Institute of Geological Science of the National Academy of Sciences of Ukraine
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Co-publisher's ISBN-13 (24)
ISBN-978-617-8521-00-4