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Geomagnetic paleointensity during Cenozoic reversals. / Sergienko, E. S.; Shashkanov, V. A.

In: Izvestiya - Physics of the Solid Earth, Vol. 35, No. 6, 01.06.1999, p. 497-505.

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

Harvard

Sergienko, ES & Shashkanov, VA 1999, 'Geomagnetic paleointensity during Cenozoic reversals', Izvestiya - Physics of the Solid Earth, vol. 35, no. 6, pp. 497-505.

APA

Sergienko, E. S., & Shashkanov, V. A. (1999). Geomagnetic paleointensity during Cenozoic reversals. Izvestiya - Physics of the Solid Earth, 35(6), 497-505.

Vancouver

Sergienko ES, Shashkanov VA. Geomagnetic paleointensity during Cenozoic reversals. Izvestiya - Physics of the Solid Earth. 1999 Jun 1;35(6):497-505.

Author

Sergienko, E. S. ; Shashkanov, V. A. / Geomagnetic paleointensity during Cenozoic reversals. In: Izvestiya - Physics of the Solid Earth. 1999 ; Vol. 35, No. 6. pp. 497-505.

BibTeX

@article{f90311bc2f224dfabd0904a675cd2c17,
title = "Geomagnetic paleointensity during Cenozoic reversals",
abstract = "The results of geomagnetic paleointensity determinations from two sections of sedimentary rocks (Chauda and Eldari sections in Georgia) are presented. These sections record the Late Tvera-Tvera, Tvera-Gilbert, and Jaramillo-Matuyama geomagnetic reversals, as well as stable intervals of the Tvera and late Matuyama subchrons. The Kamikatsura global event and an excursion are identified in a stable interval of the late Matuyama subchron recorded in the Chauda section. It was established that, irrespective of the direction (N → R or R → N) and even the class of the phenomenon (reversal, event, or excursion), all of the geomagnetic polarity transitions show common features in the behavior of paleointensity.",
author = "Sergienko, {E. S.} and Shashkanov, {V. A.}",
year = "1999",
month = jun,
day = "1",
language = "English",
volume = "35",
pages = "497--505",
journal = "Izvestiya, Physics of the Solid Earth",
issn = "1069-3513",
publisher = "Pleiades Publishing",
number = "6",

}

RIS

TY - JOUR

T1 - Geomagnetic paleointensity during Cenozoic reversals

AU - Sergienko, E. S.

AU - Shashkanov, V. A.

PY - 1999/6/1

Y1 - 1999/6/1

N2 - The results of geomagnetic paleointensity determinations from two sections of sedimentary rocks (Chauda and Eldari sections in Georgia) are presented. These sections record the Late Tvera-Tvera, Tvera-Gilbert, and Jaramillo-Matuyama geomagnetic reversals, as well as stable intervals of the Tvera and late Matuyama subchrons. The Kamikatsura global event and an excursion are identified in a stable interval of the late Matuyama subchron recorded in the Chauda section. It was established that, irrespective of the direction (N → R or R → N) and even the class of the phenomenon (reversal, event, or excursion), all of the geomagnetic polarity transitions show common features in the behavior of paleointensity.

AB - The results of geomagnetic paleointensity determinations from two sections of sedimentary rocks (Chauda and Eldari sections in Georgia) are presented. These sections record the Late Tvera-Tvera, Tvera-Gilbert, and Jaramillo-Matuyama geomagnetic reversals, as well as stable intervals of the Tvera and late Matuyama subchrons. The Kamikatsura global event and an excursion are identified in a stable interval of the late Matuyama subchron recorded in the Chauda section. It was established that, irrespective of the direction (N → R or R → N) and even the class of the phenomenon (reversal, event, or excursion), all of the geomagnetic polarity transitions show common features in the behavior of paleointensity.

UR - http://www.scopus.com/inward/record.url?scp=0040714158&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:0040714158

VL - 35

SP - 497

EP - 505

JO - Izvestiya, Physics of the Solid Earth

JF - Izvestiya, Physics of the Solid Earth

SN - 1069-3513

IS - 6

ER -

ID: 39851807