A Béli-hegység földtana és geomorfológiája másfél évszázadnyi kutatás tükrében = Geology and geomorphology of the Béli Mountains in the light of 150 years of research

Géczi, Róbert: A Béli-hegység földtana és geomorfológiája másfél évszázadnyi kutatás tükrében = Geology and geomorphology of the Béli Mountains in the light of 150 years of research. Táj, környezet és társadalom : ünnepi tanulmányok Keveiné Bárány Ilona professzor asszony tiszteletére. pp. 213-224. (2006)

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Abstract

This paper attempts to summarize the studies made in the last almost two centuries concerning the geology and geography of Codru Moma Mountains. It is clear that within the Alpine structure of the Apuseni Mountains the Codru Moma Mountains has been divided in several lithotectonic assemblages, named according to each nappe name (Biharia Nappe System, Transylvanian Nappe System, Codru Nappe System and the Bihor autochthon). Much uncertainty still remained regarding the spatial extension, the relationship between the volcanic product and the Mesozoic sedimentary deposits, further complicated by the structure of the area, and the dimension and genetics of the truncated surfaceses.

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