首页 | 本学科首页   官方微博 | 高级检索  
     检索      


Geomagnetic Field Intensity during the Neolith in the Central East European Plain
Authors:I?E?Nachasova  Email author" target="_blank">O?V?PilipenkoEmail author  G?P?Markov  S?K?Gribov  Yu?B?Tsetlin
Institution:1.Schmidt Institute of Physics of the Earth,Russian Academy of Sciences,Moscow,Russia;2.Borok Geophysical Observatory,Russian Academy of Sciences,Borok, Yaroslavl oblast,Russia;3.Institute of Archeology,Russian Academy of Sciences,Moscow,Russia
Abstract:The conducted archeomagnetic studies resulted in data on variations in the geomagnetic field intensity in the central East European Plain (Sakhtysh I site area, ? = 56°48′ N, λ = 40°33′ E) during the time interval of 5–3 ka BC. The geomagnetic field intensity varied mainly within the range of 30–60 μT. In the first half of the 5th millennium BC, the mean level of geomagnetic field intensity was about 35 μT. In the second half of the 5th–early 4th millennium BC, it rose to about 50 μT and then decreased again to reach a mean value of about 40 μT in the period of 4–3 ka BC. Comparison of the geomagnetic field intensity variation based on the obtained data and the data on the Caucasus region for the same time interval demonstrates a certain similarity.
Keywords:
本文献已被 SpringerLink 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号