MINERAL PHASES OF THE THERMAL TRANSFORMATION OF A MIXTURE OF SIDERITE AND MARTITE ORE ACCORDING TO STRUCTURAL AND MAGNETIC METHODS

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

The conducted study of thermal transformations of a mixture of siderite and martite ore in different environments showed the possibility of obtaining less altered magnetite Mag1 with a Curie point of 553 and Mag2 with TC=400 oC close to magnesia magnetite. In addition, during such transformations, impurity ferromagnetic phases close to natural maghemite (TС ~ 600 oC) and lougufengite (TС ~ 200 оС) appear. It was established that such phases are formed by simple mixing, dry and wet grinding, but as a result of thermal transformation, Mag1 and Mag2 are always formed with an approximate phase ratio of 3 to 1.


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

152-156

Published

August 15, 2024

Details about this monograph

Co-publisher's ISBN-13 (24)

ISBN-978-617-8521-00-4