Standard

Geomagnetic field fine structure for the last 30 kyr based on the magnetization of the Barents Sea sediments. / Gooskova, E. G.; Raspopov, O. M.; Piskarev, A. L.; Dergachev, V. A.; Mörner, N. A.

In: Geomagnetism and Aeronomy, Vol. 44, No. 4, 01.07.2004, p. 510-516.

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

Harvard

Gooskova, EG, Raspopov, OM, Piskarev, AL, Dergachev, VA & Mörner, NA 2004, 'Geomagnetic field fine structure for the last 30 kyr based on the magnetization of the Barents Sea sediments', Geomagnetism and Aeronomy, vol. 44, no. 4, pp. 510-516.

APA

Gooskova, E. G., Raspopov, O. M., Piskarev, A. L., Dergachev, V. A., & Mörner, N. A. (2004). Geomagnetic field fine structure for the last 30 kyr based on the magnetization of the Barents Sea sediments. Geomagnetism and Aeronomy, 44(4), 510-516.

Vancouver

Gooskova EG, Raspopov OM, Piskarev AL, Dergachev VA, Mörner NA. Geomagnetic field fine structure for the last 30 kyr based on the magnetization of the Barents Sea sediments. Geomagnetism and Aeronomy. 2004 Jul 1;44(4):510-516.

Author

Gooskova, E. G. ; Raspopov, O. M. ; Piskarev, A. L. ; Dergachev, V. A. ; Mörner, N. A. / Geomagnetic field fine structure for the last 30 kyr based on the magnetization of the Barents Sea sediments. In: Geomagnetism and Aeronomy. 2004 ; Vol. 44, No. 4. pp. 510-516.

BibTeX

@article{50192db0cc004500b103fceaa9bcd154,
title = "Geomagnetic field fine structure for the last 30 kyr based on the magnetization of the Barents Sea sediments",
abstract = "The fine temporal structure of the geomagnetic field for the past 30 kyr manifests itself in the development of geomagnetic field excursions (sharp geomagnefic pole displacements in latitude and longitude) and in slow variations in the geomagnetic field elements. An analysis of the paleomagnetic characteristics of the Barents bottom sediments shows the Etrussia-Sterno (2300-3000 years ago) and Solovki (4500-7500 years ago) geomagnetic field excursions, the Gothenburg, excursion at the Holocene-Pleistocene boundary (12-13 kyr ago) marking the end of the last glaciation, and the Mono excursion (26-28 kyr ago). A significant increase in the magnetic susceptibility at the Holocene-Pleistocene boundary, observed in eight Barents columns, reflects climate changes during this period. The cyclic component of the variation in the geomagnetic field inclination with a period of about 15 kyr has been revealed.",
author = "Gooskova, {E. G.} and Raspopov, {O. M.} and Piskarev, {A. L.} and Dergachev, {V. A.} and M{\"o}rner, {N. A.}",
year = "2004",
month = jul,
day = "1",
language = "English",
volume = "44",
pages = "510--516",
journal = "Geomagnetism and Aeronomy",
issn = "0016-7932",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "4",

}

RIS

TY - JOUR

T1 - Geomagnetic field fine structure for the last 30 kyr based on the magnetization of the Barents Sea sediments

AU - Gooskova, E. G.

AU - Raspopov, O. M.

AU - Piskarev, A. L.

AU - Dergachev, V. A.

AU - Mörner, N. A.

PY - 2004/7/1

Y1 - 2004/7/1

N2 - The fine temporal structure of the geomagnetic field for the past 30 kyr manifests itself in the development of geomagnetic field excursions (sharp geomagnefic pole displacements in latitude and longitude) and in slow variations in the geomagnetic field elements. An analysis of the paleomagnetic characteristics of the Barents bottom sediments shows the Etrussia-Sterno (2300-3000 years ago) and Solovki (4500-7500 years ago) geomagnetic field excursions, the Gothenburg, excursion at the Holocene-Pleistocene boundary (12-13 kyr ago) marking the end of the last glaciation, and the Mono excursion (26-28 kyr ago). A significant increase in the magnetic susceptibility at the Holocene-Pleistocene boundary, observed in eight Barents columns, reflects climate changes during this period. The cyclic component of the variation in the geomagnetic field inclination with a period of about 15 kyr has been revealed.

AB - The fine temporal structure of the geomagnetic field for the past 30 kyr manifests itself in the development of geomagnetic field excursions (sharp geomagnefic pole displacements in latitude and longitude) and in slow variations in the geomagnetic field elements. An analysis of the paleomagnetic characteristics of the Barents bottom sediments shows the Etrussia-Sterno (2300-3000 years ago) and Solovki (4500-7500 years ago) geomagnetic field excursions, the Gothenburg, excursion at the Holocene-Pleistocene boundary (12-13 kyr ago) marking the end of the last glaciation, and the Mono excursion (26-28 kyr ago). A significant increase in the magnetic susceptibility at the Holocene-Pleistocene boundary, observed in eight Barents columns, reflects climate changes during this period. The cyclic component of the variation in the geomagnetic field inclination with a period of about 15 kyr has been revealed.

UR - http://www.scopus.com/inward/record.url?scp=4444368903&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:4444368903

VL - 44

SP - 510

EP - 516

JO - Geomagnetism and Aeronomy

JF - Geomagnetism and Aeronomy

SN - 0016-7932

IS - 4

ER -

ID: 36844674