Geomagnetic field intensity variations during the second millennium BCE: new data from the greek middle and late bronze age

被引:0
|
作者
Aidona, E. [1 ]
Kondopoulou, D. [1 ]
Kyriakidou, E. -G. [1 ]
Camps, P. [2 ,3 ]
Sarafidis, C. [4 ]
Polymeris, G. S. [5 ]
Orgeolet, R. [6 ]
机构
[1] Aristotle Univ Thessaloniki, Sch Geol, Dept Geophys, Thessaloniki 54124, Greece
[2] Univ Montpellier, Dept Geosci, F-34095 Montpellier, France
[3] CNRS, F-34095 Montpellier, France
[4] Aristotle Univ Thessaloniki, Sch Phys, Dept Appl & Environm Phys, Thessaloniki 54124, Greece
[5] NCSR Demokritos, Inst Nanosci & Nanotechnol, Athens 15310, Greece
[6] Aix Marseille Univ, CNRS, CCJ, Aix En Provence, France
关键词
EARTHS MAGNETIC-FIELD; SECULAR VARIATION; NEAR-EAST; CONSTRAINTS; CERAMICS; PALEOINTENSITY; EUROPE; SITES; KILNS;
D O I
10.1016/j.pepi.2022.106958
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The archaeointensity records from Greece present several gaps in the prehistoric period among which the ones in the third and second millennia BCE (Early and Middle Bronze Age) are not justified by the abundance of relevant settlements in the broader Greek area. Their excavations yielded numerous collections of pottery and ceramics, well-studied to a big extent from archaeological and archaeometric point of view. We collected six groups of fragments dated from 2200 BCE to 1500 BCE which were subjected to a classical archaeomagnetic study. The material response to the experiments was mostly satisfactory, and the archaeointensity was calculated both with Thellier-Thellier and multispecimen protocols. These results, complemented by the ones recently published for the period 1500-900 BCE, and plotted versus the existing secular variation curves for Greece and relevant geomagnetic field models document a slight intensity maximum around 1900 BCE.
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页数:14
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