Tudor Berza

TL;DR: In this article, the authors describe the Banatitic Magmatic and Metallogenetic Belt (BMMB) as a narrow elongated body which runs discontinously from the Apuseni Mountains in the North, to the western part of the South Carpathians (Banat) in Romania, and further South to the Carpathian of East Serbia and still further East to Srednogorie (Bulgaria).

TL;DR: A structural study, including a kinematic analysis based on sense of shear criteria recorded in fault rocks, is combined with fission track dating in this article, for the major tectonic units which constitute the Southern Carpathians of the Parang mountains area Upper Cretaceous top-to-SSE nappe stacking was followed by WSW-ENE orogen-parallel extension in the Eocene Topto-the-ENE shearing in lower greenschist-facies mylonites from the eastern part of the Danubian window (Parang

TL;DR: The Apuseni-Banat-Timok-Srednogorie magmatic-metallogenic belt (ABTS) as discussed by the authors is a large metallogenic province in the Balkan-South Carpathian system in southeastern Europe.

TL;DR: The main terrains involved in the Cretaceous-Tertiary tectonism in the South Carpathians segment of the European Alpine orogen are the Getic-Supragetic and Danubian continental crust fragments separated by the Severin oceanic crust-floored basin this paper.

TL;DR: In this paper, the authors show that the amphibolites of the Danubian nappes are similar to the early Pan-African juvenile terranes of the Sahara, and they also confirm the existence of Late Precambrian partly juvenile terrains within the basement of the South Carpathians.