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 |
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container_title | Russian journal of Pacific geology |
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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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Geol</stitle><date>2024-08-01</date><risdate>2024</risdate><volume>18</volume><issue>4</issue><spage>436</spage><epage>451</epage><pages>436-451</pages><issn>1819-7140</issn><eissn>1819-7159</eissn><abstract>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. 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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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