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NORTHERNMOST HORST IN THE NEOALPINE -HORSTS AND GRABENS- STRUCTURE OF THE WESTERN CARPATHIANS (TATRA AND RUZBACHY HORSTS IN THE NORTHERN SLOVAKIA) IN MAGNETOTELLURIC DATA

Vladimír Bezák

First published: 2018-06-20https://doi.org/10.5593/sgem2018/1.1/s05.114View metrics

Abstract

A number of small mountain ranges (horsts) separated by small basins (grabens) with Tertiary sedimentary filling appeared in the Western Carpathians mostly in their NW and N part. The Tatry Mts. and smaller so called Ru?bachy ?island? are the northernmost horsts from a series of Western Carpathian horsts. Our magnetotelluric measurements focusing particularly on the nature of the Sub-Tatra fault and the interconnection of the Tatry Mts. with the Ru?bachy ?island? confirm steep dip of Sub-Tatra fault in the southern border of the Tatry Mts. and connection of Tatra and Ru?bachy horsts to the one transpressional structure.

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Title
NORTHERNMOST HORST IN THE NEOALPINE -HORSTS AND GRABENS- STRUCTURE OF THE WESTERN CARPATHIANS (TATRA AND RUZBACHY HORSTS IN THE NORTHERN SLOVAKIA) IN MAGNETOTELLURIC DATA
Authors
Vladimír Bezák
Proceedings
SGEM International Multidisciplinary Scientific GeoConference EXPO Proceedings; 18th International Multidisciplinary Scientific GeoConference SGEM2018, Science and Technologies in Geology, Exploration and Mining
Publisher
STEF92 Technology
Year
2018
Pages
917-924
SWS Citekey
Bezak20185917924
ISSN
1314-2704
ISBN
978-619-7408-35-5
Language
en
Publication type
Conference Paper
Keywords
Western Carpathianshorsts and grabens structuremagnetotellurics
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