The Plate Tectonic Setting of the Eocene Volcanic Belt in the Carpathian Basin

J, Csillag; Földessy, János; Zelenka, Tibor; Balazs, Emery I.

doi:10.1016/b978-0-444-99662-6.50113-1

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Periadriatic±balaton Lineament System1

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“…The easternmost member of this andesitic chain is in the NE Mµtra Mountains (Csillag et al 1980) in northern Hungary.…”

Section: Periadriatic±balaton Lineament Systemmentioning

confidence: 99%

Complex structural pattern of the Alpine-Dinaridic-Pannonian triple junction

Haas¹,

Mioč

Pamić

et al. 2000

International Journal of Earth Sciences

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Due to the political boundaries between the Central European countries, on one hand, and the thick Tertiary cover in the Pannonian Basin, on the other, the eastward continuation of the Alpine and Dinaridic units has been ambiguous and poorly documented. Based on comparative analyses, the aim of the present paper is to define the pre-Tertiary structural units in the junction area of the Alpine, Dinaridic, and Pannonian regions, in the SW part of the Pannonian Basin, and to draw conclusions on the continuation of the Alpine and Dinaridic units. According to diagnostic characteristics of the Periadriatic Lineament system, the Balaton Lineament system may be considered as its direct eastern continuation.

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“…The easternmost member of this andesitic chain is in the NE Mµtra Mountains (Csillag et al 1980) in northern Hungary.…”

Section: Periadriatic±balaton Lineament Systemmentioning

confidence: 99%