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320:. It is situated on top of the Alpine fold and thrust belt, located at the junction between the Eastern Alps, the Carpathians, and the Pannonian Basin system. The Vienna Basin has been influenced by the evolution of each of these geologic systems. The basin is characterized by four distinct tectonic phases; (1) Early
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Lee, E.Y. and
Wagreich, M. (2016) "3D visualization of the sedimentary fill and subsidence evolution in the northern and central Vienna Basin (Miocene)" Austrian Journal of Earth Sciences 109/2, 241-251,
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more than 100 years ago. The Vienna Basin fault system on which the basin lies remains seismically active. Significant earthquakes that propagated across the Vienna Basin include the
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basin formation. The basin has been studied intensively starting with classical paleontological–stratigraphical papers and then continuing since the beginning of
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408:"Polyphase tectonic subsidence evolution of the Vienna Basin inferred from quantitative subsidence analysis of the northern and central parts"
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and
Hainburg were erected at the southeastern and eastern rim as a defensive wall against attacks from the
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The Bor
Lowland and Chvojnice Hills are known collectively as Záhorská nížina (Záhorie Lowland).
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Plašienka, D., Grecula, P., Putiš, M., Kováč, M. a
Hovorka, D., 1997:
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lands downstream the Danube River. Nevertheless, the forces of King
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More than 80% of the basin area belongs to the
Austrian states of
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Evolution and structure of the
Western Carpathians: an overview.
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https://www.zobodat.at/pdf/MittGeolGes_109_2_0241-0251.pdf
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Vienna Basin proper. The part within
Czechia is called
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From the late 12th century onwards, the fortresses of
464:"Simplified Geological Map of the Weinviertel region"
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Italy, Switzerland and
Austria. A Geographical Study.
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131:. The Danube enters the basin at the Vienna Gate
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406:Lee, Eun Young; Wagreich, Michael (2017-03-01).
396:Mineralia Slovaca - Monograph, Košice, s. 1 – 24
312:The Vienna Basin formations are a series of
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335:compression and basin inversion, and (4)
272:), whilst that within Slovakia is called
99:The fairly level area has the shape of a
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412:International Journal of Earth Sciences
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230:. Along the southern and western rim,
166:entered the Vienna Basin during the
16:Sedimentary basin in Central Europe
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178:troops, who besieged the city in
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521:Geology of the Czech Republic
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210:. The northern parts on the
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316:that were deposited in the
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327:, (2) Middle–Late Miocene
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174:. It was again invaded by
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355:in the mid-4th century.
347:of 1590, and the strong
341:hydrocarbon exploration
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127:mountain ranges of the
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298:Chvojnická pahorkatina
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168:Austrian-Hungarian War
117:Little Hungarian Plain
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23:View over Vienna from
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170:in 1485 to begin the
115:separate it from the
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371:Rees, Henry (1974).
516:Geology of Slovakia
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331:, (3) Late Miocene–
270:Lower Morava Valley
222:rivers are part of
107:plateau beyond the
89:Western Carpathians
511:Geology of Austria
492:48.20556; 16.37389
314:sedimentary layers
290:) in Lower Austria
266:Dolnomoravský úval
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145:Little Carpathians
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25:Lainzer Tiergarten
255:Bad Fischau-Brunn
241:occur in several
164:Matthias Corvinus
73:sedimentary basin
61:Viedenská kotlina
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172:Siege of Vienna
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139:, it leaves at
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190:Structuring
81:Carpathians
505:Categories
478:16°22′26″E
475:48°12′20″N
359:References
349:earthquake
337:Quaternary
251:Bad Vöslau
232:geothermal
141:Devín Gate
434:1437-3262
353:Carnuntum
351:that hit
284:Marchfeld
243:spa towns
160:Hungarian
135:near Mt.
133:water gap
105:Marchfeld
95:Geography
65:Hungarian
37:‹See Tfd›
333:Pliocene
245:such as
228:Slovakia
149:Hainburg
147:east of
83:and the
322:Miocene
318:Neogene
308:Geology
280:region)
278:Záhorie
260:Parts:
239:springs
224:Czechia
176:Ottoman
143:in the
101:spindle
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218:) and
212:Morava
208:Vienna
109:Danube
79:, the
57:Slovak
41:German
247:Baden
220:Thaya
216:March
49:Czech
430:ISSN
377:ISBN
253:and
234:and
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