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326:. 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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414:"Polyphase tectonic subsidence evolution of the Vienna Basin inferred from quantitative subsidence analysis of the northern and central parts"
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109:, over an area of 50 km (31 mi) by 200 km (120 mi). In the north it stretches up to the
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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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Vienna Basin proper. The part within the Czech
Republic is called
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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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From the late 12th century onwards, the fortresses of
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Italy, Switzerland and
Austria. A Geographical Study.
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137:. The Danube enters the basin at the Vienna Gate
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412:Lee, Eun Young; Wagreich, Michael (2017-03-01).
402:Mineralia Slovaca - Monograph, Košice, s. 1 – 24
318:The Vienna Basin formations are a series of
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341:compression and basin inversion, and (4)
278:), whilst that within Slovakia is called
105:The fairly level area has the shape of a
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418:International Journal of Earth Sciences
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236:. Along the southern and western rim,
172:entered the Vienna Basin during the
27:Sedimentary basin in Central Europe
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184:troops, who besieged the city in
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527:Geology of the Czech Republic
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117:River. In the southeast, the
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216:. The northern parts on the
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322:that were deposited in the
204:Chvojnice Hills in Slovakia
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333:, (2) Middle–Late Miocene
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282:(Bor Lowland, part of the
180:. It was again invaded by
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361:in the mid-4th century.
353:of 1590, and the strong
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133:mountain ranges of the
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304:Chvojnická pahorkatina
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174:Austrian-Hungarian War
123:Little Hungarian Plain
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34:View over Vienna from
493:48.20556°N 16.37389°E
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176:in 1485 to begin the
121:separate it from the
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377:Rees, Henry (1974).
522:Geology of Slovakia
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337:, (3) Late Miocene–
276:Lower Morava Valley
113:plateau beyond the
95:Western Carpathians
517:Geology of Austria
498:48.20556; 16.37389
320:sedimentary layers
296:) in Lower Austria
272:Dolnomoravský úval
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151:Little Carpathians
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36:Lainzer Tiergarten
261:Bad Fischau-Brunn
247:occur in several
170:Matthias Corvinus
79:sedimentary basin
67:Viedenská kotlina
16:(Redirected from
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178:Siege of Vienna
162:Wiener Neustadt
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127:Gutenstein Alps
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91:Pannonian Plain
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196:Structuring
87:Carpathians
511:Categories
484:16°22′26″E
481:48°12′20″N
365:References
355:earthquake
343:Quaternary
257:Bad Vöslau
238:geothermal
147:Devín Gate
440:1437-3262
359:Carnuntum
357:that hit
290:Marchfeld
249:spa towns
166:Hungarian
141:near Mt.
139:water gap
111:Marchfeld
101:Geography
71:Hungarian
339:Pliocene
251:such as
234:Slovakia
155:Hainburg
153:east of
89:and the
328:Miocene
324:Neogene
314:Geology
286:region)
284:Záhorie
266:Parts:
245:springs
182:Ottoman
149:in the
107:spindle
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224:) and
218:Morava
214:Vienna
115:Danube
85:, the
63:Slovak
47:German
253:Baden
226:Thaya
222:March
55:Czech
436:ISSN
383:ISBN
259:and
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