Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1002/2016GL071494 |
Further evidence of the Levantine Iron Age geomagnetic anomaly from Georgian pottery | |
Shaar, Ron1; Tauxe, Lisa2; Goguitchaichvili, Avto3; Devidze, Marina4,5,6; Licheli, Vakhtang5 | |
2017-03-16 | |
发表期刊 | GEOPHYSICAL RESEARCH LETTERS |
ISSN | 0094-8276 |
EISSN | 1944-8007 |
出版年 | 2017 |
卷号 | 44期号:5 |
文章类型 | Article |
语种 | 英语 |
国家 | Israel; USA; Mexico; Georgia; Italy |
英文摘要 | Recent archaeomagnetic data from ancient Israel revealed the existence of a so-called "Levantine Iron Age geomagnetic anomaly" (LIAA) which spanned the first 350years of the first millennium before the Common Era (B.C.E.) and was characterized by a high averaged geomagnetic field (virtual axial dipole moments, VADM>140ZAm(2), nearly twice of today's field), short decadal-scale geomagnetic spikes (VADM of 160-185ZAm(2)), fast field variations, and substantial deviation from dipole field direction. The geographic constraints of the LIAA have remained elusive due to limited high-quality paleointensity data in surrounding locations. Here we report archaeointensity data from Georgia showing high field values (VADM>150ZAm(2)) in the tenth or ninth century B.C.E., low field values (VADM<60 ZAm(2)) in the twelfth century B.C.E., and fast field variation in the fifth and fourth centuries B.C.E. High field values in the time frame of LIAA have been observed so far only in three localities near the Levant: Eastern Anatolia, Turkmenistan, and now Georgia, all located east of longitude 30 degrees E. West of this, in the Balkans, field values in the same time are moderate to low. These constraints put geographic limits on the extent of the LIAA and support the hypothesis of an unusually intense regional geomagnetic anomaly during the beginning of the first half of the first millennium B.C.E., comparable in area and magnitude (but of opposite sign) to the presently active South Atlantic anomaly. |
领域 | 气候变化 |
收录类别 | SCI-E ; SSCI |
WOS记录号 | WOS:000398183700021 |
WOS关键词 | EARTHS MAGNETIC-FIELD ; INTENSITY VARIATIONS ; SECULAR VARIATION ; COOLING-RATE ; NEAR-EAST ; BRONZE ; CENTURIES ; MILLENNIA ; EUROPE |
WOS类目 | Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/27700 |
专题 | 气候变化 |
作者单位 | 1.Hebrew Univ Jerusalem, Inst Earth Sci, Jerusalem, Israel; 2.Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA; 3.Univ Nacl Autonoma Mexico, Inst Geofis, Serv Arqueomagnetico Nacl & Lab Interinstituc Mag, Morelia, Michoacan, Mexico; 4.Ivane Javakhishvili Tbilisi State Univ, M Nodia Inst Geophys, Tbilisi, Georgia; 5.Ivane Javakhishvili Tbilisi State Univ, Inst Archeol, Tbilisi, Georgia; 6.Italian Natl Res Council CNR, Inst Geosci & Earth Resources IGG CNR, Pisa, Italy |
推荐引用方式 GB/T 7714 | Shaar, Ron,Tauxe, Lisa,Goguitchaichvili, Avto,et al. Further evidence of the Levantine Iron Age geomagnetic anomaly from Georgian pottery[J]. GEOPHYSICAL RESEARCH LETTERS,2017,44(5). |
APA | Shaar, Ron,Tauxe, Lisa,Goguitchaichvili, Avto,Devidze, Marina,&Licheli, Vakhtang.(2017).Further evidence of the Levantine Iron Age geomagnetic anomaly from Georgian pottery.GEOPHYSICAL RESEARCH LETTERS,44(5). |
MLA | Shaar, Ron,et al."Further evidence of the Levantine Iron Age geomagnetic anomaly from Georgian pottery".GEOPHYSICAL RESEARCH LETTERS 44.5(2017). |
条目包含的文件 | 条目无相关文件。 |
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