Globally strong geomagnetic field intensity circa 3000 years ago SCIE SCOPUS

DC Field Value Language
dc.contributor.author Hong, Hoabin -
dc.contributor.author Yu, Yongjae -
dc.contributor.author Lee, Chan Hee -
dc.contributor.author Kim, Ran Hee -
dc.contributor.author Park, Jingyu -
dc.contributor.author Doh, Seong-Jae -
dc.contributor.author Kim, Wonnyon -
dc.contributor.author Sung, Hyongmi -
dc.date.accessioned 2020-04-20T05:25:13Z -
dc.date.available 2020-04-20T05:25:13Z -
dc.date.created 2020-01-28 -
dc.date.issued 2013-12-01 -
dc.identifier.issn 0012-821X -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/3043 -
dc.description.abstract High-fidelity geomagnetic field intensity determination was carried out using 191 baked fragments collected from 20 kilns or hearths with ages ranging between similar to 1200 BC and similar to AD 1725 in South Korea. Geomagnetic field intensity variation displayed three narrow minima at similar to 800-700 BC, similar to AD 700, and similar to AD 1600 and two maxima at similar to 1200-1100 BC and similar to AD 1000-1100. In most time intervals, virtual axial dipole moment (VADM) variation is confined within 20% of the present VADM. However, geomagnetic field intensity circa 3000 yr ago is nearly 40% larger than the present value. Such high VADMs circa 3000 yr ago are in phase with those in other longitudinal bands in northern hemisphere centered at 5E (France), 30E (the Middle East) and 200E (Hawaii). Although strong geomagnetic field intensity circa 3000 yr ago is globally synchronous, the highest VADM occurs at slightly different time intervals in different locations. Hence it is possible that the globally strong geomagnetic field intensity circa 3000 yr ago reflects the migration of persistent hemispheric flux in northern hemisphere or an episode of geomagnetic field hemispheric asymmetry. Crown Copyright (C) 2013 Published by Elsevier B.V. All rights reserved. -
dc.description.uri 1 -
dc.language English -
dc.publisher ELSEVIER SCIENCE BV -
dc.subject EARTHS MAGNETIC-FIELD -
dc.subject PAST 7 MILLENNIA -
dc.subject SECULAR VARIATION -
dc.subject WESTERN-EUROPE -
dc.subject PALEOINTENSITY METHODS -
dc.subject CHINESE CERAMICS -
dc.subject LAVA FLOWS -
dc.subject ARCHAEOMAGNETIC JERKS -
dc.subject ARCHEOINTENSITY DATA -
dc.subject DIPOLE-MOMENT -
dc.title Globally strong geomagnetic field intensity circa 3000 years ago -
dc.type Article -
dc.citation.endPage 152 -
dc.citation.startPage 142 -
dc.citation.title EARTH AND PLANETARY SCIENCE LETTERS -
dc.citation.volume 383 -
dc.contributor.alternativeName 김원년 -
dc.identifier.bibliographicCitation EARTH AND PLANETARY SCIENCE LETTERS, v.383, pp.142 - 152 -
dc.identifier.doi 10.1016/j.epsl.2013.09.043 -
dc.identifier.scopusid 2-s2.0-84886691247 -
dc.identifier.wosid 000328593500015 -
dc.type.docType Article -
dc.description.journalClass 1 -
dc.subject.keywordPlus EARTHS MAGNETIC-FIELD -
dc.subject.keywordPlus PAST 7 MILLENNIA -
dc.subject.keywordPlus SECULAR VARIATION -
dc.subject.keywordPlus WESTERN-EUROPE -
dc.subject.keywordPlus PALEOINTENSITY METHODS -
dc.subject.keywordPlus CHINESE CERAMICS -
dc.subject.keywordPlus LAVA FLOWS -
dc.subject.keywordPlus ARCHAEOMAGNETIC JERKS -
dc.subject.keywordPlus ARCHEOINTENSITY DATA -
dc.subject.keywordPlus DIPOLE-MOMENT -
dc.subject.keywordAuthor strong geomagnetic field intensity -
dc.subject.keywordAuthor archeomagnetism -
dc.subject.keywordAuthor paleointensity -
dc.subject.keywordAuthor secular variation -
dc.subject.keywordAuthor dipolar field -
dc.subject.keywordAuthor non-dipolar field -
dc.relation.journalWebOfScienceCategory Geochemistry & Geophysics -
dc.description.journalRegisteredClass scie -
dc.description.journalRegisteredClass scopus -
dc.relation.journalResearchArea Geochemistry & Geophysics -
Appears in Collections:
Marine Resources & Environment Research Division > Ocean Georesources Research Department > 1. Journal Articles
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