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Magnetic parameters and variations in the composition of igneous rocks of the Franz Josef Land archipelago. / Piskarev, A. L.; Heunemann, Ch; Makar'ev, A. A.; Makar'eva, A. M.; Bachtadse, V.; Aleksyutin, M.

In: Izvestiya, Physics of the Solid Earth, Vol. 45, No. 2, 27.02.2009, p. 150-166.

Research output: Contribution to journal › Article › peer-review

Harvard

Piskarev, AL, Heunemann, C, Makar'ev, AA, Makar'eva, AM, Bachtadse, V & Aleksyutin, M 2009, 'Magnetic parameters and variations in the composition of igneous rocks of the Franz Josef Land archipelago', Izvestiya, Physics of the Solid Earth, vol. 45, no. 2, pp. 150-166. https://doi.org/10.1134/S1069351309020050

APA

Piskarev, A. L., Heunemann, C., Makar'ev, A. A., Makar'eva, A. M., Bachtadse, V., & Aleksyutin, M. (2009). Magnetic parameters and variations in the composition of igneous rocks of the Franz Josef Land archipelago. Izvestiya, Physics of the Solid Earth, 45(2), 150-166. https://doi.org/10.1134/S1069351309020050

Vancouver

Piskarev AL, Heunemann C, Makar'ev AA, Makar'eva AM, Bachtadse V, Aleksyutin M. Magnetic parameters and variations in the composition of igneous rocks of the Franz Josef Land archipelago. Izvestiya, Physics of the Solid Earth. 2009 Feb 27;45(2):150-166. https://doi.org/10.1134/S1069351309020050

Author

Piskarev, A. L. ; Heunemann, Ch ; Makar'ev, A. A. ; Makar'eva, A. M. ; Bachtadse, V. ; Aleksyutin, M. / Magnetic parameters and variations in the composition of igneous rocks of the Franz Josef Land archipelago. In: Izvestiya, Physics of the Solid Earth. 2009 ; Vol. 45, No. 2. pp. 150-166.

BibTeX

@article{ba06444ea12e412c9d272d025c72f8f0,
title = "Magnetic parameters and variations in the composition of igneous rocks of the Franz Josef Land archipelago",
abstract = "A combined study of magnetic parameters of basalt and andesite samples is performed in the framework of geological investigations of the Franz Josef Land at the paleomagnetic laboratory of Munich University. The study included the determination of the coercivity, saturation magnetization, Curie points, natural remanent magnetization (NRM), and magnetic susceptibility and the examination of ferromagnetic minerals with a microscope. Data on the chemical composition of rocks are obtained for all samples, and radiological ages are determined for the majority of rocks. Thermomagnetic curves of samples are subdivided into four types depending on the composition of ferromagnetic NRM carriers. The data obtained point to multiple changes in the predominant composition of igneous rocks. Each stage of magmatism is characterized by a specific type of the ferromagnetic component in the rocks and, therefore, magnetomineralogical investigations can be used for differentiation and correlation of the igneous rocks.",
author = "Piskarev, {A. L.} and Ch Heunemann and Makar'ev, {A. A.} and Makar'eva, {A. M.} and V. Bachtadse and M. Aleksyutin",
year = "2009",
month = feb,
day = "27",
doi = "10.1134/S1069351309020050",
language = "English",
volume = "45",
pages = "150--166",
journal = "Izvestiya, Physics of the Solid Earth",
issn = "1069-3513",
publisher = "Pleiades Publishing",
number = "2",

}

RIS

TY - JOUR

T1 - Magnetic parameters and variations in the composition of igneous rocks of the Franz Josef Land archipelago

AU - Piskarev, A. L.

AU - Heunemann, Ch

AU - Makar'ev, A. A.

AU - Makar'eva, A. M.

AU - Bachtadse, V.

AU - Aleksyutin, M.

PY - 2009/2/27

Y1 - 2009/2/27

N2 - A combined study of magnetic parameters of basalt and andesite samples is performed in the framework of geological investigations of the Franz Josef Land at the paleomagnetic laboratory of Munich University. The study included the determination of the coercivity, saturation magnetization, Curie points, natural remanent magnetization (NRM), and magnetic susceptibility and the examination of ferromagnetic minerals with a microscope. Data on the chemical composition of rocks are obtained for all samples, and radiological ages are determined for the majority of rocks. Thermomagnetic curves of samples are subdivided into four types depending on the composition of ferromagnetic NRM carriers. The data obtained point to multiple changes in the predominant composition of igneous rocks. Each stage of magmatism is characterized by a specific type of the ferromagnetic component in the rocks and, therefore, magnetomineralogical investigations can be used for differentiation and correlation of the igneous rocks.

AB - A combined study of magnetic parameters of basalt and andesite samples is performed in the framework of geological investigations of the Franz Josef Land at the paleomagnetic laboratory of Munich University. The study included the determination of the coercivity, saturation magnetization, Curie points, natural remanent magnetization (NRM), and magnetic susceptibility and the examination of ferromagnetic minerals with a microscope. Data on the chemical composition of rocks are obtained for all samples, and radiological ages are determined for the majority of rocks. Thermomagnetic curves of samples are subdivided into four types depending on the composition of ferromagnetic NRM carriers. The data obtained point to multiple changes in the predominant composition of igneous rocks. Each stage of magmatism is characterized by a specific type of the ferromagnetic component in the rocks and, therefore, magnetomineralogical investigations can be used for differentiation and correlation of the igneous rocks.

UR - http://www.scopus.com/inward/record.url?scp=60749137436&partnerID=8YFLogxK

U2 - 10.1134/S1069351309020050

DO - 10.1134/S1069351309020050

M3 - Article

AN - SCOPUS:60749137436

VL - 45

SP - 150

EP - 166

JO - Izvestiya, Physics of the Solid Earth

JF - Izvestiya, Physics of the Solid Earth

SN - 1069-3513

IS - 2

ER -

ID: 36844439