Geomagnetic Field Intensity during the Neolith in the Central East European Plain


如何引用文章

全文:

开放存取 开放存取
受限制的访问 ##reader.subscriptionAccessGranted##
受限制的访问 订阅存取

详细

The conducted archeomagnetic studies resulted in data on variations in the geomagnetic field intensity in the central East European Plain (Sakhtysh I site area, ϕ = 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.

作者简介

I. Nachasova

Schmidt Institute of Physics of the Earth

Email: pilipenko@ifz.ru
俄罗斯联邦, Moscow

O. Pilipenko

Schmidt Institute of Physics of the Earth

编辑信件的主要联系方式.
Email: pilipenko@ifz.ru
俄罗斯联邦, Moscow

G. Markov

Schmidt Institute of Physics of the Earth

Email: pilipenko@ifz.ru
俄罗斯联邦, Moscow

S. Gribov

Borok Geophysical Observatory

Email: pilipenko@ifz.ru
俄罗斯联邦, Borok, Yaroslavl oblast

Yu. Tsetlin

Institute of Archeology

Email: pilipenko@ifz.ru
俄罗斯联邦, Moscow

补充文件

附件文件
动作
1. JATS XML

版权所有 © Pleiades Publishing, Ltd., 2018