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STRUCTURE OF THE GEOMAGNETIC FIELD IN CORRELATION WITH NEOTECTONIC REGIONALIZATION OF THE REPUBLIC OF MACEDONIA

Blagoj Delipetrev

First published: 2011-06-20https://doi.org/10.5593/sgem2011/s06.122View metrics

Abstract

The paper presents research of the structure of the geomagnetic field in correlation with the neotectonic regionalization. The territo ry of the Republic of Macedonia, according to the neotectonic processes, is divided in three zones: Western - Macedonian zone which include Alpine orogeny and Pelagonian massif, Vardar zone and Eastern - Macedonian zone which is part of the old Paleozioc rock mass on the Balkan Peninsula. Anomalous geomagnetic field on the territory of the Republic of Macedonia is presented with regional and local components. Selection of the repeat stations density and the method for data processing is adapted to separate the regional from the local component of the anomalous geomagnetic field. The paper presents maps of the elements of the regional anomalous geomagnetic field and the map of the Z - component for the local field.

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Publication details

Title
STRUCTURE OF THE GEOMAGNETIC FIELD IN CORRELATION WITH NEOTECTONIC REGIONALIZATION OF THE REPUBLIC OF MACEDONIA
Authors
Blagoj Delipetrev
Proceedings
SGEM International Multidisciplinary Scientific GeoConference EXPO Proceedings; SGEM2011 11th International Multidisciplinary Scientific GeoConference
Publisher
Stef92 Technology
Year
2011
Pages
Not available yet
ISSN
1314-2704
ISBN
Not available yet
Language
en
Publication type
Conference Paper
Keywords
regional geomagnetic fieldanomalous fieldlocal fieldneotectonic structurecorrelation
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