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


Cite item

Full Text

Open Access Open Access
Restricted Access Access granted
Restricted Access Subscription Access

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, 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.

About the authors

I. E. Nachasova

Schmidt Institute of Physics of the Earth

Email: pilipenko@ifz.ru
Russian Federation, Moscow

O. V. Pilipenko

Schmidt Institute of Physics of the Earth

Author for correspondence.
Email: pilipenko@ifz.ru
Russian Federation, Moscow

G. P. Markov

Schmidt Institute of Physics of the Earth

Email: pilipenko@ifz.ru
Russian Federation, Moscow

S. K. Gribov

Borok Geophysical Observatory

Email: pilipenko@ifz.ru
Russian Federation, Borok, Yaroslavl oblast

Yu. B. Tsetlin

Institute of Archeology

Email: pilipenko@ifz.ru
Russian Federation, Moscow

Supplementary files

Supplementary Files
Action
1. JATS XML

Copyright (c) 2018 Pleiades Publishing, Ltd.