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Foreland basin north of the Alps
Molasse basin (or North Alpine foreland basin) is a foreland basin north of the Alps which formed during the Oligocene and Miocene epochs. The basin formed
Molasse_basin
Sedimentary rock deposit associated with the formation of mountain chains
marine deposits in front of rising mountain chains. The molasse deposits accumulate in a foreland basin, especially on top of flysch-like deposits, for example
Molasse
deposits (flysch and molasse) are found. This Bavarian and Swiss foreland basin is called the Molasse basin. The foreland basin deposits are overthrust
Geology_of_the_Alps
Thrust belt
particularly in the south, by the Cenozoic molasse of the North Alpine foreland basin, also known as the Swiss Molasse Basin. Studied since the 18th century, the
Geology_of_the_Jura_Massif
Structural basin that develops adjacent and parallel to a mountain belt
this point, the basin enters the overfilled stage and deposition of terrestrial clastic sediments occurs. These are known as molasse. Sediment fill within
Foreland_basin
Extinct species of ladybug
Coccinellidae. It was discovered in Oeningen, in Sarmatian age limestone of the Molasse basin in Germany. "†Coccinella amabilis Heer 1864". Paleobiology Database
Coccinella_amabilis
Regions of long-term subsidence creating space for infilling by sediments
sedimentary basin even if it is no longer a bathymetric or topographic depression. The Williston Basin, Molasse basin and Magallanes Basin are examples
Sedimentary_basin
Tectonic plate which includes most of Eurasia
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
Eurasian_plate
Extinct species of whale
Physeterula dubusi. It was found in the Alpine town of Stockach in the Molasse basin, which was a coastal area with strong tidal currents. The remains of
Orcinus_meyeri
together with the Odenwald, the Spessart, the Black Forest and the Molasse Basin) and the Upper Rhine Graben. South of the South German Block and the
Geology_of_Germany
Molasse basin in southwest Germany
Saar–Nahe Basin is a molasse basin in southwest Germany. The basin is located south of the Hunsrück mountains between the rivers Nahe and the Saar. The
Saar–Nahe_Basin
Formation of the Alpine mountain ranges of Europe, the Middle East and northwest Africa
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
Alpine_orogeny
Microcontinent in the Paleozoic era
Baltica–Avalonia convergence based on the sedimentary record of a foreland basin". Terra Nova. 30 (1): 8–16. Bibcode:2018TeNov..30....8M. doi:10.1111/ter
Avalonia
Prehistoric shallow inland sea in Eurasia
stages the Molasse basin north of the Alps; the Vienna Basin, the Outer Carpathian Basin, the Pannonian Basin, and further east to the basin of the current
Paratethys
– the first thrust belt to be recognised by geologists. London Basin Hampshire Basin North Downs Weald South Downs London-Brabant Massif Cornubian batholith
Geology_of_Great_Britain
Herbivorous mammal
Jean-Pierre (2011-03-17). "Tapiridae (Perissodactyla, Mammalia) of the Swiss Molasse Basin during the Oligocene–Miocene transition". Journal of Vertebrate Paleontology
Tapir
Extinct giant shark species
preserved vertebral column of a single specimen, excavated in the Antwerp Basin, Belgium, in 1926. It comprises 150 vertebral centra, with the centra ranging
Megalodon
Flood retention basin in Canton of Zurich
21 km². From a geological point of view, Affoltern lies within the Molasse Basin of the Swiss Plateau, which accumulated sediments composed of the eroded
Jonenbach flood retention basin
Jonenbach_flood_retention_basin
Difference between ideal and observed gravitational acceleration at a location
an ancient continental collision. The low-density sediments of the Molasse basin produce a negative anomaly. Larger surveys across the region provide
Gravity_anomaly
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
Geology_of_Ireland
Sea between Africa, Asia, and Europe
characterizing the landscape are the Rhône-Saône valley, the Jura Mountains, the Molasse basin and the northwestern slopes of the Alps. "San Marino". Encyclopædia
Mediterranean_Sea
Long narrow depression bordering the Aegean Sea to the south
be so) are located in the southern outer Hellenides. Meanwhile, the deep basins of the Trench and their marine ecologies are the homes of a number of marine
Hellenic_Trench
Low-lying flatland region encompassing the northern part of the Caspian Sea
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
Caspian_Depression
Oil field in Russia
The Timan-Pechora Basin is a sedimentary basin located between Timan Ridge and the Ural Mountains in northern Russia. The basin contains oil and gas fields
Timan-Pechora_Basin
Serbia and is mostly covered in the north by the sediments of the Pannonian Basin. Outcrops can be found in the Fruška Gora (Fruška mountains). Here the unit
Geology_of_Serbia
Pleistocene outwash plain in Bavaria, Germany
surroundings are built. These most recent deposits overlie the Neogene Molasse basin of the Alpine Foreland, which by contrast comprises fine-grained fluviatile
Munich_gravel_plain
faulting in the Mesozoic with the opening of Mediterranean-style oceanic basins. Romanian Geological Survey borehole data was used to map the Moesian Platform
Moesian_plate
Fold belt of west and central Europe, formed during the Hercynian orogeny
When a foreland basin was formed in the Rhenohercynian zone, this was filled with upper Carboniferous (Pennsylvanian) flysch and molasse sediments. The
Rhenohercynian_Zone
"Helvetic nappes" are a nappe stack that was thrust over the molasse of the Molasse basin in the Alpine foreland. They are composed of Mesozoic marine
Helvetic_(geology)
century. In Scotland these rocks are found predominantly in the Moray Firth basin and Orkney Archipelago, and along the southern margins of the Highland Boundary
Geology_of_Scotland
Extinct great ape from Miocene Europe
rhinoceros Aceratherium. The site is located in the Upper Freshwater Molasse of the Molasse basin; by the late Miocene, the Paratethys Sea had dried up and the
Danuvius_guggenmosi
Hyblean plateau on land to the offshore Gela basin of southwestern Sicily. Based on fossil analysis, the basin has been developing since Late Pliocene; its
Geology_of_Sicily
Trough, Epirus-Akarnania basin and Cycladic Basin are all examples of molasse basins from the early Miocene. The Ionian Islands basin is part of the Preapulian
Geology_of_Greece
Since then the basin has been deepened mainly through subsidence caused by extensional tectonics. In the northern part of the Baltic Sea basin, including
Geology_of_the_Baltic_Sea
Orogenic belt in southwestern Sweden and southern Norway
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
Sveconorwegian_orogeny
Geology of peninsula in southwestern Europe
The Ponga Nappe Province is to the east of the Central Coal Basin, Stephanian age molasse deposits overlie the other Carboniferous rocks and are unrelated
Geology of the Iberian Peninsula
Geology_of_the_Iberian_Peninsula
basement rocks disappear under the Mesozoic cover of the Aquitaine basin and the Paris Basin. This somewhat simplistic model is locally disturbed by fault
Geology_of_the_Massif_Central
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
Karelides
Geological rifts by the Alps
Miocene before resuming in the Late Miocene. The eastern margin of the basin was overridden by thrust faults from the Jura Mountains, the leading edge
European_Cenozoic_Rift_System
Geological salt deposit in Franche-Comté, France, formed during the Late Triassic
décollée sur des couches d'évaporites [Geology of the Central Jura and the Molasse Basin: New Insights into an Evaporite-Based Foreland Fold and Thrust Belt]
Franche-Comté_saltwater_basin
Ancient tectonic plate from the Cambrian to the Carboniferous Period
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
Baltic_plate
Continental tectonic plate comprising most of the Anatolian Peninsula (Asia Minor)
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
Anatolian_plate
of piggyback basins. The Tannheim-Losenstein basin in the Eastern Alps is a deep marine piggyback basin. Molasse basin – Foreland basin north of the Alps
Piggyback_basin
The southwest shield of the East European craton
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
Ukrainian_Shield
Swiss geologist and academic
foreland basins, and passive continental margins. He has worked on Alpine tectonics, including the Jura Mountains and the Swiss Molasse Basin, as well
Jon_Mosar
Small tectonic plate in the eastern Mediterranean Sea
formation of a back-arc basin. This environment has created a number of horst and graben features on the seafloor, similar to basin and range topography
Aegean_Sea_plate
Region in Bavaria, Germany
basement, lying beneath the Tertiary and Quaternary deposits of the molasse basin, and the still visible part northwest of this line, which belongs to
Bavarian_Forest
Geology of the country of Armenia
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
Geology_of_Armenia
lies beneath the Sicily Channel, separating the Ionian Basin from the western Mediterranean Basin. The islands lie around 200 km to the south of the subduction
Geology_of_Malta
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
Geology_of_Guernsey
drive of the African Plate into the Eurasian Plate in the Mediterranean basin is the most prominent aspect of the European scene today. The pressure exerted
Geology_of_Europe
Small tectonic plate now part of the Eurasian plate
anticlockwise relative to Eurasia. This caused the subduction of the Ligurian Basin onto the eastern side. This formed the Betic nappe stack. After 85 Ma the
Iberian_plate
Part of the river Rhine in Switzerland and Germany
meander at Rheinau. In its eastern portion, the river passes through the Molasse basin (passing south of the Hegau region), while in its western part it traverses
High_Rhine
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
Geology_of_Andorra
Geology of Europe
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
East_European_Craton
Field Trip Guide, prepared for Statoil Faroes Licence Groups by Volcanic Basin Petroleum Research, Nordic Volcanological Institute and Iceland National
Geology_of_Iceland
European tectonic zone
intramontane basins filled with Rotliegend sediments and older deposits. The Eger Graben in the northwest of the Czech Republic and the Saar-Nahe Basin in western
Saxothuringian_Zone
Part of the East European Craton
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
Sarmatian_Craton
Orogeny took place in late Devon. During Carboniferous and Permian, rift basins were formed. Carboniferous strata are found along Billefjorden, and Permian
Geology_of_Svalbard
Small tectonic plate in the Mediterranean
window Flysch zone Giudicárie line Greywacke zone Hohe Tauern window Molasse basin Penninic thrustfront Periadriatic Seam Ivrea zone Lepontin dome Rechnitz
Adriatic_plate
Geological feature in Eastern Europe
from the Ural Mountains to the Tornquist Zone and from the Peri-Caspian Basin to the Barents Sea. Over geological time the platform area has experienced
East_European_Platform
the main rifting phase in the Central Graben, Viking Graben, More Basin, Vøring Basin and on the Barents shelf. This was also the period of deposition
Geology_of_Norway
Small tectonic unit in the Pannonian Basin in Europe
tectonic unit. It is situated in the Pannonian Basin in Europe. The Carpathian Mountains and the basin surrounded by them were formed from the Cretaceous
Pelso_plate
the Terek Basin. The Caspian Basin is a system of basins and platforms. It is divided into smaller basins, in the North, the North Caspian Basin. The north
Geology_of_Russia
Block of late Neoproterozoic crust which underlies the Midlands region of England
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
Midlands_Microcraton
during the early Jurassic. The Harstad, Tromsø, Bjørnøya and Sørvestsnaget basins all developed during the late Jurassic and into the Cretaceous as the rifting
Geology_of_the_Norwegian_Sea
Geological events that formed the Ural Mountains
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
Uralian_orogeny
Former piece of oceanic crust that is seen as part of the Tethys Ocean
The Piemont-Liguria basin or the Piemont-Liguria Ocean (sometimes only one of the two names is used, for example: Piemonte Ocean) was a former piece of
Piemont-Liguria_Ocean
Piece of continental crust in the Penninic nappes of the Alps
window Flysch zone Giudicárie line Greywacke zone Hohe Tauern window Molasse basin Penninic thrustfront Periadriatic Seam Ivrea zone Lepontin dome Rechnitz
Briançonnais_zone
times. During the Caledonian orogeny, Finland was likely a sunken foreland basin covered by sediments; subsequent uplift and erosion would have eroded all
Geology_of_Finland
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
Geology_of_the_Faroe_Islands
faulting of the existing rock sequence, most particularly within the Welsh Basin, a process which intensified northwards. Parts of the sequence were subjected
Geology_of_Wales
Superfamily of mammals
Jean-Pierre (2011). "Tapiridae (Perissodactyla, Mammalia) of the Swiss Molasse Basin during the Oligocene–Miocene transition". Journal of Vertebrate Paleontology
Tapiroidea
Collective Noun
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
Hellenic_orogeny
The Ebro Basin, the drainage basin of the River Ebro, encompasses much of the northeast quarter of the Iberian Peninsula, in Spain. It formed during the
Ebro_Basin
Microcontinent or group of continental fragments rifted away from Gondwana
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
Armorican_terrane
Geographic region, Southern Germany
the influence of the ice ages and has a rich variety of landforms. A molasse basin of extensive Tertiary and Quaternary sediments —silt and clay, sand
Alpine_Foreland
The Moscow Basin is a major sedimentary basin and tectonic structural feature in the stable East European Craton. It has been widely studied by Russian
Moscow_Basin
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
Volgo–Uralia
Geological description of the Jersey Island
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
Geology_of_Jersey
Geologic massif in the Swiss Alps
window Flysch zone Giudicárie line Greywacke zone Hohe Tauern window Molasse basin Penninic thrustfront Periadriatic Seam Ivrea zone Lepontin dome Rechnitz
Aarmassif
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
Geology_of_Cyprus
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
Dnieper-Donets_Rift
Type of electricity generation system
normal faults as geothermal exploration targets in the Western Bavarian Molasse Basin: Case study Mauerstetten". Zeitschrift der Deutschen Gesellschaft für
Enhanced_geothermal_system
South-Armorican south-vergent thrusts. The Basque-Cantabrian Basin is a large sedimentary basin on thinned continental crust that lies onshore and offshore
Geology_of_the_Bay_of_Biscay
south-east. In the south-west they disappear below recent sediments of the Po basin that are lying discordant on top of them. The Southern Alps are composed
Southern_Alps_(Europe)
European regional geology
jointed, epicontinental Mesozoic sediments covered and hidden by Miocene molasse sediments. The east–west and northwest–southeast-striking fold sets interfere
Geology_of_the_Pyrenees
Genus of fishes
Uganda, the Democratic Republic of the Congo, Niger, and Sudan), France (Molasse basin), Saudi Arabia, and Slovakia. Earlier specimens from the Eocene are
Lates
Study of geologic regions
interfingering facies change in sedimentary deposits when discussing a sedimentary basin system, or the leading or boundary thrust of an orogen. Geology of Africa
Regional_geology
Köprüçay, and Manavgat Basins together make up the Antalya Basin. On the north side, the basins include the axial Tauride molasse basin as well as the Çameli
Isparta_Angle
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
Limagne_Graben
Geological formation in the Pennine Alps
window Flysch zone Giudicárie line Greywacke zone Hohe Tauern window Molasse basin Penninic thrustfront Periadriatic Seam Ivrea zone Lepontin dome Rechnitz
Dent_Blanche_nappe
Mountain building event in northern Europe
Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift
Scandian_orogeny
Sedimentary basin in the Barents Sea
71°N 46°E / 71°N 46°E / 71; 46 The Barents Basin or East Barents Basin is a sedimentary basin underlying the eastern half of the Barents Sea. Lying
Barents_Basin
The Mezen Basin is a sedimentary basin located in northwestern Russia. It list southeast of the White Sea and bounds the Timanide Orogen to the north and
Mezen_Basin
Geologic formation in Austria
Oligocene gastropods and bivalves from the Lower and Upper Austrian Molasse Basin", Österreichische Akademie der Wissenschaften, Schriftenreihe der
Pielach_Formation
North Sea. It acts as source rock for oil fields in the West Netherlands Basin. During late Jurassic times the Zuidwal volcano was active in a now submerged
Geology_of_the_Netherlands
Geological structures thrust north by Alps orogeny
In Switzerland, Germany and Austria they are also thrust over the Molasse basin of the Alpine foreland. In turn, the Helvetic nappes were overthrust
Helvetic_nappes
Trace fossil
229–253 Arp, Gernot (2008). "Stop 7: Tufa oncoids of the river Moosach, Molasse Basin". In Reitner, Joachim; Quéric, Nadia-Valérie; Reich, Mike (eds.). Geobiology
Oncolite
There are two basins the large South Permian Basin, and the smaller Northern Permian basin, which are east–west trending. The basins are separated by
Geology_of_the_North_Sea
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