Umfang:
Online-Ressource (XXII, 244 p. 213 illus., 60 illus. in color, digital)
ISBN:
9783642219108
Serie:
Regional Geology Reviews
Inhalt:
Hungary lies in the central part of the Pannonian Basin, surrounded by the ranges of the Alps, Carpathians, and Dinarides. The geology of the country can be summarized as a process whereby complicated plate collision-type orogeny was followed by the formation of a young basin in which a relatively complete sequence of basin infill has been preserved. The handbook "Geology of Hungary" presents an outline of the main features of the geology and geohistory of the region in a single volume, illustrated by a great number of color figures and photos for the benefit of foreign geoscientists intereste
Anmerkung:
Description based upon print version of record
,
Geology of Hungary; Contents; Introduction; History of Geologic Research; Geography and Outline of Geologic Framework; Structural Units and Main Stages of the Structural Evolution; 1:Geology and History of Evolution of the ALCAPA Mega-Unit; 1.1 Austroalpine Units; 1.1.1 Lower Austroalpine Nappe System; Sopron Mountains; Fertőrákos (Mörbisch) ``Schist-Island´´; 1.1.2 Upper Austroalpine Nappe System; 1.1.3 Penninic Unit; 1.2 Central and Internal Western Carpathian Units; 1.2.1 Veporic Unit; 1.2.2 Zemplénic Unit; 1.2.3 Internal Western Carpathian Nappe-Stack; 1.2.3.1 Bódva Nappe
,
1.2.3.2 Torna Nappe1.2.3.3 Telekesoldal Nappe; 1.2.3.4 Szőlősardó Unit; 1.2.3.5 Silica-Aggtelek Nappe; Evaporitic Sole (Tornakápolna Unit); Permian-Earliest Triassic Evaporites; Siliciclastic Ramp in the Early Triassic; Restricted Shelf in the Latest Early Triassic and Earliest Anisian; Carbonate Ramp and Platform Evolution in the Middle to Early Late Triassic; Expansion of Deep-Sea Environments in the Late Triassic-Early Jurassic; 1.3 Pelso Composite Unit; 1.3.1 Transdanubian Range Unit; 1.3.1.1 Variscan Evolutionary Cycle; Balaton Phyllite Group (Ordovician-Lower Devonian)
,
Devonian Deep and Shallow Marine Carbonate FormationsLower Carboniferous Shallow Marine Deposits; Post-orogenic Continental Molasse in the Late Carboniferous; Post-Variscan Granitoids; 1.3.1.2 Alpine Evolutionary Cycle; Transgression in the Middle-Late Permian; Early Triassic Siliciclastic-Carbonate Ramp; Anisian Carbonate Ramp; Mid-Triassic Platform Dissection and Volcanism; Basin Infilling in the Carnian; Late Triassic Carbonate Platform Evolution; Segmentation of Carbonate Platforms in the Early Jurassic; Deep Pelagic Sediment Deposition in the Toarcian-Late Jurassic Interval
,
Early Cretaceous BasinsMaiolica Basin in the Bakony Area; Siliciclastic Basin in the Gerecse Area; Albian-Cenomanian Cycle; Senonian Cycle; 1.3.2 Mid-Transdanubian Unit; 1.3.2.1 South Karavank Unit; 1.3.2.2 Julian-Savinja Unit; 1.3.2.3 South Zala and Kalnik Units; 1.3.3 Bükk Composite Unit; 1.3.3.1 Bükk Unit ss.; Nagyfennsík Unit; Variscan Evolutionary Cycle; Post-Variscan Marine Molasse Stage; Alpine Evolutionary Cycle; Middle-Late Permian Coastal Plain and Carbonate Ramp; P/Tr Boundary Event and Early Triassic Siliciclastic-Carbonate Ramp; Carbonate Platform in the Anisian
,
Middle Triassic Volcanic ActivityCarbonate Platforms and Intraplatform Basins in the Ladinian; Siliciclastic Sediment Deposition and Volcanic Activity in the Carnian; Late Triassic Carbonate Platforms and Intraplatform Basins; Deep-Sea Basins in the Jurassic; Szarvaskő Unit; 1.3.3.2 Szendrő Unit; Abod Subunit; Rakaca Subunit; 1.3.3.3 Uppony Unit; Tapolcsány Subunit; Lázbérc Subunit; Late Cretaceous Gravity Flow Deposits; 1.4 Accretion of the ALCAPA Mega-Unit; 1.4.1 Paratethys Evolution and Its Consequences for the Palaeogene-Neogene Chronostratigraphic Framework
,
1.4.2 Hungarian Palaeogene Basin
Weitere Ausg.:
ISBN 9783642219092
Weitere Ausg.:
Buchausg. u.d.T. Geology of Hungary Berlin, Heidelberg [u.a.] : Springer, 2012 ISBN 3642219098
Weitere Ausg.:
ISBN 9783642219092
Sprache:
Englisch
Fachgebiete:
Geowissenschaften
,
Geographie
Schlagwort(e):
Ungarn
;
Geologie
;
Ungarn
;
Geologie
DOI:
10.1007/978-3-642-21910-8
URL:
Volltext
(lizenzpflichtig)
