FERROMAGNETIC PHASES OF MAGNETITE QUARTZITES ACCORDING TO THERMOMAGNETOMETRY AND FERROMAGNETIC RESONANCE DATA

Authors

T.S. Antonenko , M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the National Academy of Sciences of Ukraine; V.P. Snisar , M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the National Academy of Sciences of Ukraine; O.A. Kalinichenko , M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the National Academy of Sciences of Ukraine; M.M. Bagmut , M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the National Academy of Sciences of Ukraine; V.V. Ovsienko , M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the National Academy of Sciences of Ukraine; A.M. Kalinichenko , M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the National Academy of Sciences of Ukraine

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

Details about this monograph

Co-publisher's ISBN-13 (24)

ISBN-978-617-8521-00-4