[HTML][HTML] Orogenic architecture of the Mediterranean region and kinematic reconstruction of its tectonic evolution since the Triassic

DJJ Van Hinsbergen, TH Torsvik, SM Schmid… - Gondwana …, 2020 - Elsevier
The basins and orogens of the Mediterranean region ultimately result from the opening of
oceans during the early break-up of Pangea since the Triassic, and their subsequent …

The formation and deformation of the Neogene Pannonian basin: a structural overview

L Csontos, I Dunkl, B Koroknai, G Tari… - Geological Society …, 2025 - lyellcollection.org
The Pannonian Basin is a continental back-arc basin. Palaeomagnetics defined three
terranes: Alcapa (Alps–Carapathians–Pannonian), Tisza–Dacia and Dinarides, rotated …

Mesozoic plate tectonic reconstruction of the Carpathian region

L Csontos, A Vörös - Palaeogeography, Palaeoclimatology, Palaeoecology, 2004 - Elsevier
Palaeomagnetic, palaeobiogeographic and structural comparisons of different parts of the
Alpine–Carpathian region suggest that four terranes comprise this area: the Alcapa, Tisza …

On the formation and evolution of the Pannonian Basin: Constraints derived from the structure of the junction area between the Carpathians and Dinarides

L Matenco, D Radivojević - Tectonics, 2012 - Wiley Online Library
The large number and distribution of rollback systems in Mediterranean orogens infer the
possibility of interacting extensional back‐arc deformation driven by different slabs. The …

The Mid-Hungarian line: a zone of repeated tectonic inversions

L Csontos, A Nagymarosy - Tectonophysics, 1998 - Elsevier
The Mid-Hungarian line is a major tectonic feature of the Intra-Carpathian area separating
two terranes of different origin and tectonic structure. Although this tectonic line was known …

Tectonic, magmatic, and metallogenic evolution of the Late Cretaceous arc in the Carpathian‐Balkan orogen

D Gallhofer, A Quadt, I Peytcheva, SM Schmid… - …, 2015 - Wiley Online Library
Abstract The Apuseni‐Banat‐Timok‐Srednogorie Late Cretaceous magmatic arc in the
Carpathian‐Balkan orogen formed on the European margin during closure of the Neotethys …

[图书][B] Alpine tectonics of the Pannonian Basin

GC Tari - 1994 - search.proquest.com
Allowing for the palinspastic restoration of Tertiary strike-slip and extensional faulting it is
concluded that the Pannonian Basin is superposed on a Middle Cretaceous thrust and fold …

Upper Cretaceous magmatic series and associated mineralisation in the Carpathian–Balkan Orogen

T Berza, E Constantinescu, SN Vlad - Resource Geology, 1998 - Wiley Online Library
The Alpine Orogen contains in South East Europe, from the Carpathians to the Balkans–
Srednogorie, an Upper Cretaceous, ore bearing igneous belt: a narrow elongated body …

Tertiary subduction and slab break-off model of the Carpathian–Pannonian region

M Nemcok, L Pospisil, J Lexa, RA Donelick - Tectonophysics, 1998 - Elsevier
This paper illustrates the application of multidisciplinary data analysis to the Carpathian–
Pannonian region and presents a new Tertiary development model that incorporates all …

Regional setting and geochronology of the Late Cretaceous banatitic magmatic and metallogenetic belt

CL Ciobanu, NJ Cook, H Stein - Mineralium Deposita, 2002 - Springer
The 1,500-km-long Banatitic Magmatic and Metallogenetic Belt (BMMB) of Romania, Serbia
and Bulgaria is a complex calc-alkaline magmatic arc of Late Cretaceous age. It hosts a …