Holocene Geomagnetic Excursions in Peat Deposits

The paper presents the results of comprehensive (microprobe, paleomagnetic and magnetic) studies on peats from the Tyapka peat section (Russian Far East). Radiocarbon dating placed the start of peat formation at ∼11.7 ky B.P. The principle carriers of magnetization were found to be magnetite, to a l...

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Veröffentlicht in:Russian journal of Pacific geology 2024-08, Vol.18 (4), p.436-451
Hauptverfasser: Peskov, A. Yu, Didenko, A. N., Karetnikov, A. S., Klimin, M. A., Arkhipov, M. V., Kozhemyako, N. V., Tikhomirova, A. I.
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container_end_page 451
container_issue 4
container_start_page 436
container_title Russian journal of Pacific geology
container_volume 18
creator Peskov, A. Yu
Didenko, A. N.
Karetnikov, A. S.
Klimin, M. A.
Arkhipov, M. V.
Kozhemyako, N. V.
Tikhomirova, A. I.
description The paper presents the results of comprehensive (microprobe, paleomagnetic and magnetic) studies on peats from the Tyapka peat section (Russian Far East). Radiocarbon dating placed the start of peat formation at ∼11.7 ky B.P. The principle carriers of magnetization were found to be magnetite, to a lesser extent hematite and, possibly, greigite. The relative paleointensity values obtained through calculations are in good agreement with the literature data. Intervals with negative inclinations of the magnetization vector were identified in peats, which most likely correspond to geomagnetic excursions in the Holocene. The research constrained the duration of the geomagnetic excursions, as well as the geomagnetic field intensity behavior not typical for such variations.
doi_str_mv 10.1134/S1819714024700143
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source SpringerNature Journals
subjects Earth and Environmental Science
Earth Sciences
Geology
Geomagnetic field
Greigite
Haematite
Holocene
Magnetite
Palaeomagnetism
Paleomagnetism
Peat
Radiocarbon dating
title Holocene Geomagnetic Excursions in Peat Deposits
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