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Metallic Iron in Basalts of the Malyi Yenisei Lava River: Results of Thermomagnetic Study

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dc.contributor Казанский федеральный университет
dc.contributor.author Pechersky Diamar
dc.contributor.author Kazansky Alexei
dc.contributor.author Kozlovsky Alexander
dc.contributor.author Kuzina Dilyara Mtygullovna
dc.contributor.author Markov Gennadiy
dc.date.accessioned 2020-09-28T08:50:59Z
dc.date.available 2020-09-28T08:50:59Z
dc.date.issued 2020
dc.identifier.citation Pechersky, D.M. Metallic Iron in Basalts of the Malyi Yenisei Lava River: Results of Thermomagnetic Study / D.M. Pechersky, A.Y. Kazansky, A.M. Kozlovsky, D.M. Kuzina, G.P. Markov // Izvestiya, Physics of the Solid Earth. - Vol. 56. - No. 4. - P. 461-469.
dc.identifier.uri https://dspace.kpfu.ru/xmlui/handle/net/159401
dc.description.abstract This paper shows that the mineral composition of dolerites affects their specific paramagnetic susceptibility. Two methods for calculating the specific paramagnetic susceptibility were proposed: one used the thermomagnetic analysis (TMA) curve and the other the Mi(B) curve. There was no significant difference between the results obtained with these two approaches. Application of the proposed methods to dolerite core samples showed that specific paramagnetic susceptibility can be used as the basis for correlation of sills. The composition of titanomagnetites in dolerites can be used as an accessory parameter.
dc.language.iso en
dc.relation.ispartofseries Izvestiya, Physics of the Solid Earth
dc.rights открытый доступ
dc.subject dolerites
dc.subject specific paramagnetic susceptibility
dc.subject titanomagnetites
dc.subject sill
dc.subject thermomagnetic curves
dc.subject.other Геология
dc.subject.other Геофизика
dc.title Metallic Iron in Basalts of the Malyi Yenisei Lava River: Results of Thermomagnetic Study
dc.type Article
dc.contributor.org Институт геологии и нефтегазовых технологий
dc.description.pages 461-469
dc.relation.ispartofseries-issue 4
dc.relation.ispartofseries-volume 56
dc.pub-id 238729
dc.identifier.doi 10.1134/S1069351320030076


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