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The molasse can sometimes completely fill a foreland basin, creating a nearly flat depositional surface, that nonetheless remains a structural
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that form as terrestrial or shallow marine deposits in front of rising mountain chains. The molasse deposits accumulate in a
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of lowlands, as compared to deep-water flysch sediments. Sedimentation stops when the
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Type of sedimentary rock deposit associated with the formation of mountain chains.
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Tenchov, Yanaki G. (1989) "Demarcation of
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