Improvements in Archaeomagnetic Dating in Western Europe from the Late Bronze to the Late Iron Ages: An Alternative to the Problem of the Hallstattian Radiocarbon Plateau

被引:28
|
作者
Herve, G. [1 ,4 ]
Lanos, P. [2 ,3 ]
机构
[1] Ludwig Maximilians Univ Munchen, Dept Geo & Umweltwissensch, Theresienstr 41, D-80333 Munich, Germany
[2] Univ Bordeaux Montaigne, CNRS, UMR 5060, IRAMAT CRP2A, Bordeaux, France
[3] Univ Rennes 1, CNRS, UMR 6118, Geosci Rennes, Rennes, France
[4] Aix Marseille Univ, CNRS, IRD, CEREGE, Aix En Provence, France
关键词
archaeomagnetism; archaeomagnetic dating; Bayesian modelling; directional secular variation of geomagnetic field; Western Europe; Iron Age; Late Bronze Age; EARTHS MAGNETIC-FIELD; SECULAR VARIATION CURVES; ARCHAEOINTENSITY; CALIBRATION; CENTURIES; MILLENNIA; DIRECTION; FRANCE; SITE; BC;
D O I
10.1111/arcm.12344
中图分类号
K85 [文物考古];
学科分类号
0601 ;
摘要
We present a new curve of the directional secular variation of the geomagnetic field in Western Europe between 1500 bce and 200 ce. Its computation relies on a Bayesian framework. The fast secular variation during the Late Bronze and Early Iron Ages makes archaeomagnetic dating efficient with a respective precision of 150-200 and 60-100years during these periods. The Bayesian method also provides posterior date distributions that refine the dating of reference data, especially during the period of the Hallstattian radiocarbon plateau. Archaeomagnetism becomes a valuable alternative to radiocarbon and will help to improve the archaeological chronologies.
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页码:870 / 883
页数:14
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