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Low-Temperature Magnetic Properties and Magnetic Mineralogy of the Ropruchey Sill (Russian Karelia). / Kosterov, Andrei ; Sergienko, Elena S. ; Kharitonskii, Petr V. ; Yanson, Svetlana Yu. ; Vasilieva, Irina A. .

Recent Advances in Rock Magnetism, Environmental Magnetism and Paleomagnetism: International Conference on Geomagnetism, Paleomagnetism and Rock Magnetism (Kazan, Russia). ред. / D.K. Nurgaliev; V.P. Shcherbakov; A. Kosterov; S. Spassov. Cham : Springer Nature, 2019. стр. 205-223 (Springer Geophysics ).

Результаты исследований: Публикации в книгах, отчётах, сборниках, трудах конференций › статья в сборнике › научная › Рецензирование

Harvard

Kosterov, A, Sergienko, ES, Kharitonskii, PV, Yanson, SY & Vasilieva, IA 2019, Low-Temperature Magnetic Properties and Magnetic Mineralogy of the Ropruchey Sill (Russian Karelia). в DK Nurgaliev, VP Shcherbakov, A Kosterov & S Spassov (ред.), Recent Advances in Rock Magnetism, Environmental Magnetism and Paleomagnetism: International Conference on Geomagnetism, Paleomagnetism and Rock Magnetism (Kazan, Russia). Springer Geophysics , Springer Nature, Cham, стр. 205-223. https://doi.org/10.1007/978-3-319-90437-5_16

APA

Kosterov, A., Sergienko, E. S., Kharitonskii, P. V., Yanson, S. Y., & Vasilieva, I. A. (2019). Low-Temperature Magnetic Properties and Magnetic Mineralogy of the Ropruchey Sill (Russian Karelia). в D. K. Nurgaliev, V. P. Shcherbakov, A. Kosterov, & S. Spassov (Ред.), Recent Advances in Rock Magnetism, Environmental Magnetism and Paleomagnetism: International Conference on Geomagnetism, Paleomagnetism and Rock Magnetism (Kazan, Russia) (стр. 205-223). (Springer Geophysics ). Springer Nature. https://doi.org/10.1007/978-3-319-90437-5_16

Vancouver

Kosterov A, Sergienko ES, Kharitonskii PV, Yanson SY, Vasilieva IA. Low-Temperature Magnetic Properties and Magnetic Mineralogy of the Ropruchey Sill (Russian Karelia). в Nurgaliev DK, Shcherbakov VP, Kosterov A, Spassov S, Редакторы, Recent Advances in Rock Magnetism, Environmental Magnetism and Paleomagnetism: International Conference on Geomagnetism, Paleomagnetism and Rock Magnetism (Kazan, Russia). Cham: Springer Nature. 2019. стр. 205-223. (Springer Geophysics ). https://doi.org/10.1007/978-3-319-90437-5_16

Author

Kosterov, Andrei ; Sergienko, Elena S. ; Kharitonskii, Petr V. ; Yanson, Svetlana Yu. ; Vasilieva, Irina A. . / Low-Temperature Magnetic Properties and Magnetic Mineralogy of the Ropruchey Sill (Russian Karelia). Recent Advances in Rock Magnetism, Environmental Magnetism and Paleomagnetism: International Conference on Geomagnetism, Paleomagnetism and Rock Magnetism (Kazan, Russia). Редактор / D.K. Nurgaliev ; V.P. Shcherbakov ; A. Kosterov ; S. Spassov. Cham : Springer Nature, 2019. стр. 205-223 (Springer Geophysics ).

BibTeX

@inbook{70fd816aaa824f2896a7f0cce141b202,
title = "Low-Temperature Magnetic Properties and Magnetic Mineralogy of the Ropruchey Sill (Russian Karelia)",
abstract = "We report low-temperature magnetic properties of predominantly mafic rocks from the Mesoproterozoic Ropruchey sill, Karelia. Based on microscopic observations, the studied rocks can be classified into two groups, granodiorites and gabbro-diorites, with different magnetic mineralogy. In granodiorites, the only magnetic mineral is stoichiometric magnetite characterized by a Verwey transition temperature of 120–121 K. In gabbro-diorites, the magnetic mineralogy is also dominated by magnetite, which however contains 2–3% of Ti substitution atoms, lowering the Verwey transition temperature to 94–103 K. In addition, the gabbro-diorites appear to contain some amount of a more Ti-rich titanomagnetite, as well as another, yet unidentified magnetic phase, manifesting itself by a peculiar temperature and frequency-dependent behavior of magnetic susceptibility.",
keywords = "Low-temperature magnetometry, Magnetite, Verwey transition, Scanning electron microscopy, Microanalysis",
author = "Andrei Kosterov and Sergienko, {Elena S.} and Kharitonskii, {Petr V.} and Yanson, {Svetlana Yu.} and Vasilieva, {Irina A.}",
year = "2019",
doi = "10.1007/978-3-319-90437-5_16",
language = "English",
isbn = "9783319904368",
series = "Springer Geophysics ",
publisher = "Springer Nature",
pages = "205--223",
editor = "D.K. Nurgaliev and Shcherbakov, {V.P. } and A. Kosterov and S. Spassov",
booktitle = "Recent Advances in Rock Magnetism, Environmental Magnetism and Paleomagnetism",
address = "Germany",

}

RIS

TY - CHAP

T1 - Low-Temperature Magnetic Properties and Magnetic Mineralogy of the Ropruchey Sill (Russian Karelia)

AU - Kosterov, Andrei

AU - Sergienko, Elena S.

AU - Kharitonskii, Petr V.

AU - Yanson, Svetlana Yu.

AU - Vasilieva, Irina A.

PY - 2019

Y1 - 2019

N2 - We report low-temperature magnetic properties of predominantly mafic rocks from the Mesoproterozoic Ropruchey sill, Karelia. Based on microscopic observations, the studied rocks can be classified into two groups, granodiorites and gabbro-diorites, with different magnetic mineralogy. In granodiorites, the only magnetic mineral is stoichiometric magnetite characterized by a Verwey transition temperature of 120–121 K. In gabbro-diorites, the magnetic mineralogy is also dominated by magnetite, which however contains 2–3% of Ti substitution atoms, lowering the Verwey transition temperature to 94–103 K. In addition, the gabbro-diorites appear to contain some amount of a more Ti-rich titanomagnetite, as well as another, yet unidentified magnetic phase, manifesting itself by a peculiar temperature and frequency-dependent behavior of magnetic susceptibility.

AB - We report low-temperature magnetic properties of predominantly mafic rocks from the Mesoproterozoic Ropruchey sill, Karelia. Based on microscopic observations, the studied rocks can be classified into two groups, granodiorites and gabbro-diorites, with different magnetic mineralogy. In granodiorites, the only magnetic mineral is stoichiometric magnetite characterized by a Verwey transition temperature of 120–121 K. In gabbro-diorites, the magnetic mineralogy is also dominated by magnetite, which however contains 2–3% of Ti substitution atoms, lowering the Verwey transition temperature to 94–103 K. In addition, the gabbro-diorites appear to contain some amount of a more Ti-rich titanomagnetite, as well as another, yet unidentified magnetic phase, manifesting itself by a peculiar temperature and frequency-dependent behavior of magnetic susceptibility.

KW - Low-temperature magnetometry

KW - Magnetite

KW - Verwey transition

KW - Scanning electron microscopy

KW - Microanalysis

U2 - 10.1007/978-3-319-90437-5_16

DO - 10.1007/978-3-319-90437-5_16

M3 - Article in an anthology

SN - 9783319904368

T3 - Springer Geophysics

SP - 205

EP - 223

BT - Recent Advances in Rock Magnetism, Environmental Magnetism and Paleomagnetism

A2 - Nurgaliev, D.K.

A2 - Shcherbakov, V.P.

A2 - Kosterov, A.

A2 - Spassov, S.

PB - Springer Nature

CY - Cham

ER -

ID: 39218719