[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 …

Mesozoic igneous suites in Hungary: Implications for genesis and tectonic setting in the northwestern part of Tethys

S Harangi, C Szabó, S Józsa, Z Szoldán… - International Geology …, 1996 - Taylor & Francis
Mesozoic igneous rocks occur in various tectonic units of the Intra-Carpathian Area of
Eastern Europe. These rocks were situated several hundred km apart from one another …

The connection between iron ore formations and “mud-shrimp” colonizations around sunken wood debris and hydrothermal sediments in a Lower Cretaceous …

V Jáger, F Molnár, D Buchs, P Koděra - Earth-Science Reviews, 2012 - Elsevier
In the Early Cretaceous, the continental rift basin of the Mecsek Mts.(Hungary), was situated
on the southern edge of the European plate. The opening of the North Atlantic Ocean …

Geochemistry and petrogenesis of the Early Cretaceous continental rift-type volcanic rocks of the Mecsek Mountains, South Hungary

S Harangi - Lithos, 1994 - Elsevier
Early Cretaceous volcanic rocks (basanite to phonolite) from the Mecsek Mountains (South
Hungary) represent the products of Late Mesozoic extension-related alkaline magmatism at …

Geology and history of evolution of the Tisza mega-unit

T Szederkényi, J Haas, A Nagymarosy, G Hámor - Geology of Hungary, 2012 - Springer
Abstract The Tisza Mega-unit (Tisia Terrane) forms the basement of the Pannonian Basin
south of the Mid-Hungarian Lineament (see Fig. 1 in “Introduction”). In the territory of …

Geology and history of evolution of the ALCAPA Mega-Unit

T Szederkényi, S Kovács, J Haas, A Nagymarosy - Geology of Hungary, 2012 - Springer
The ALCAPA Mega-unit (composite terrane) consists of elements of the Austroalpine and
Penninic Units (Eastern Alps), the Central and Inner Western Carpathian Units, and the …

Nature of the magma source of the Szarvaskö Complex (NE-Hungary): Petrological and geochemical constraints

M Aigner-Torres, F Koller - Ofioliti, 1999 - ofioliti.it
The Szarvaskö complex exposes a rare fragment of Jurassic mafic and ultramafic igneous
rocks that have been described as a dismembered portion of a Mesozoic ophiolitic …

[PDF][PDF] Petrology and palaeotectonic setting of Cretaceous alkaline basaltic volcanismin the Pieniny Klippen Belt (Western Carpathians, Slovakia)

J Spišiak, D Plašienka, J Bucova, T Mikuš - Geological Quarterly, 2011 - bibliotekanauki.pl
Occurrences of mafic alkaline volcanics are scattered all around Europe, being mostly
related to anorogenic, extensional tectonic environments. While the widespread Cenozoic …

Genesis of carbonate aggregates in lamprophyres from the northeastern Transdanubian Central Range, Hungary: Magmatic or hydrothermal origin?

T Azbej, C Szabó, RJ Bodnar, G Dobosi - Mineralogy and Petrology, 2006 - Springer
Summary Carbonate aggregates in Late Cretaceous lamprophyre dikes of the northeastern
Transdanubian Central Range (TCR) in Northwest Hungary have been classified into three …

The Budaörs-1 well revisited: Contributions to the Triassic stratigraphy, sedimentology, and magmatism of the southwestern part of the Buda Hills

J Haas, T Budai, I Dunkl, É Farics, S Józsa… - Central European …, 2017 - akjournals.com
The 1,200-m-deep Budaörs-1 borehole provided important data for our understanding of the
stratigraphy and tectonic setting of the southern part of the Buda Hills. Although previous …