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Als Molassebecken, auch Voralpentrog, wird … Als Molassebecken, auch Voralpentrog, wird in der regionalen Geologie der Alpenländer der von Molassesedimenten eingenommene Bereich am Alpennordrand bezeichnet. Der Begriff Molassebecken wird aber auch allgemein auf ein Sedimentbecken bezogen, das den Verwitterungsschutt eines aufsteigenden Gebirges aufnimmt. Das hier behandelte nordalpine Molassebecken wird unterteilt in einen größeren nördlichen Bereich, die Vorlandmolasse mit Gesteinen in überwiegend ungestörter Lagerung, und einen schmaleren südlichen Bereich unmittelbar am Alpennordrand, die Subalpine Molasse (Molassezone, Faltenmolasse) mit verschuppten und steilgestellten Molassegesteinen.pten und steilgestellten Molassegesteinen.
, Het Molassebekken is een in het Oligoceen … Het Molassebekken is een in het Oligoceen en Mioceen gevormd voorlandbekken ten noorden van de Alpen. Het bekken ontstond als gevolg van de flexuur (ombuiging) van de Europese plaat onder het gewicht van de destijds ten zuiden van het bekken vormende Alpen. Het bekken is gevuld met molasse, het materiaal dat door erosie en denudatie uit een vormend gebergte wordt verwijderd en door rivieren wordt afgevoerd. De naam "molassebekken" kan in de geologie ook in algemene betekenis gebruikt worden voor een gelijktijdig met een gebergte gevormd voorlandbekken van het type dat ten noorden van de Alpen ligt. Het bekken is de typelocatie van molasse, een opvolging van sedimentaire gesteentelagen bestaande uit conglomeraat en zandsteen, die alleen voorkomt langs de rand van gebergten.leen voorkomt langs de rand van gebergten.
, The Molasse basin (or North Alpine forelan … The 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 as a result of the flexure of the European plate under the weight of the orogenic wedge of the Alps that was forming to the south. In geology, the name "molasse basin" is sometimes also used in a general sense for a synorogenic (formed contemporaneously with the orogen) foreland basin of the type north of the Alps. The basin is the type locality of molasse, a sedimentary sequence of conglomerates and sandstones, material that was removed from the developing mountain chain by erosion and denudation, that is typical for foreland basins.tion, that is typical for foreland basins.
, Il bacino della Molassa è un bacino di ava … Il bacino della Molassa è un bacino di avampaese situato nelle Alpi Nord-orientali, formatosi durante l'Oligocene e il Miocene come risultato della flessione della placca euroasiatica sotto il peso del prisma di accrezione orogenetica delle Alpi che si stavano formando a sud. In geologia, il termine bacino della molassa viene a volte utilizzato anche in senso più generale per indicare un bacino di avampaese postorogenico, dove si accumulano i sedimenti di demolizione di una catena montuosa. Il bacino è la località tipo della molassa, una sequenza di materiale conglomerato sedimentario e di arenaria, rimossi per erosione dalle montagne in formazione.per erosione dalle montagne in formazione.
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Het Molassebekken is een in het Oligoceen … Het Molassebekken is een in het Oligoceen en Mioceen gevormd voorlandbekken ten noorden van de Alpen. Het bekken ontstond als gevolg van de flexuur (ombuiging) van de Europese plaat onder het gewicht van de destijds ten zuiden van het bekken vormende Alpen. Het bekken is gevuld met molasse, het materiaal dat door erosie en denudatie uit een vormend gebergte wordt verwijderd en door rivieren wordt afgevoerd.rwijderd en door rivieren wordt afgevoerd.
, Als Molassebecken, auch Voralpentrog, wird … Als Molassebecken, auch Voralpentrog, wird in der regionalen Geologie der Alpenländer der von Molassesedimenten eingenommene Bereich am Alpennordrand bezeichnet. Der Begriff Molassebecken wird aber auch allgemein auf ein Sedimentbecken bezogen, das den Verwitterungsschutt eines aufsteigenden Gebirges aufnimmt.utt eines aufsteigenden Gebirges aufnimmt.
, Il bacino della Molassa è un bacino di ava … Il bacino della Molassa è un bacino di avampaese situato nelle Alpi Nord-orientali, formatosi durante l'Oligocene e il Miocene come risultato della flessione della placca euroasiatica sotto il peso del prisma di accrezione orogenetica delle Alpi che si stavano formando a sud. In geologia, il termine bacino della molassa viene a volte utilizzato anche in senso più generale per indicare un bacino di avampaese postorogenico, dove si accumulano i sedimenti di demolizione di una catena montuosa.nti di demolizione di una catena montuosa.
, The Molasse basin (or North Alpine forelan … The 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 as a result of the flexure of the European plate under the weight of the orogenic wedge of the Alps that was forming to the south.of the Alps that was forming to the south.
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Molassebecken
, Bacino della Molassa
, Molasse basin
, Molassebekken
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