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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). ed. / D.K. Nurgaliev; V.P. Shcherbakov; A. Kosterov; S. Spassov. Cham : Springer Nature, 2019. p. 205-223 (Springer Geophysics ).

Research output: Chapter in Book/Report/Conference proceeding › Article in an anthology › peer-review

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). in DK Nurgaliev, VP Shcherbakov, A Kosterov & S Spassov (eds), Recent Advances in Rock Magnetism, Environmental Magnetism and Paleomagnetism: International Conference on Geomagnetism, Paleomagnetism and Rock Magnetism (Kazan, Russia). Springer Geophysics , Springer Nature, Cham, pp. 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). In D. K. Nurgaliev, V. P. Shcherbakov, A. Kosterov, & S. Spassov (Eds.), Recent Advances in Rock Magnetism, Environmental Magnetism and Paleomagnetism: International Conference on Geomagnetism, Paleomagnetism and Rock Magnetism (Kazan, Russia) (pp. 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). In Nurgaliev DK, Shcherbakov VP, Kosterov A, Spassov S, editors, Recent Advances in Rock Magnetism, Environmental Magnetism and Paleomagnetism: International Conference on Geomagnetism, Paleomagnetism and Rock Magnetism (Kazan, Russia). Cham: Springer Nature. 2019. p. 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). editor / D.K. Nurgaliev ; V.P. Shcherbakov ; A. Kosterov ; S. Spassov. Cham : Springer Nature, 2019. pp. 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