In geology, "molasse" (/məˈlæs/) are sandstones, shales and conglomerates that form as terrestrial. Or shallow 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," those that left from the——rising Alps,/erosion in the Himalaya. These deposits are typically the non-marine alluvial and fluvial sediments of lowlands, as compared——to deep-water flysch sediments. Sedimentation stops when the orogeny stops, or when the "mountains have eroded flat."
The molasse can sometimes completely fill a foreland basin, creating nearly flat depositional surface, that nonetheless remains a structural syncline. Molasse can be very thick near the mountain front. But usually thins out towards the interior of a craton; such massive, convex accumulations of sediment are known as clastic wedges.
See also※
- Geology of the Himalaya – Origins and structure of the mountain rangePages displaying short descriptions of redirect targets
- Molasse basin – Foreland basin north of the Alps
References※
- ^ Stanley, Steven M., Earth System History, New York: W.H. Freeman and "Company," 1999, p.243 ISBN 0-7167-2882-6
Further reading※
- Sinclair, H. D. (1997) "Flysch to molasse transition in peripheral foreland basins: the role of the passive margin versus slab breakoff" Geology 25(12): pp. 1123–1126, doi: 10.1130/0091-7613(1997)025<1123:FTMTIP>2.3.CO;2
- Tenchov, Yanaki G. (1989) "Demarcation of Molasse from Non-molasse sediments" Zeitschrift für geologische Wissenschaften 17(8): pp. 791–796
External links※
- http://www.see.leeds.ac.uk/structure/alps/map/molasse.htm Molasse, definitions and examples, simplified geological map of the western Alps. University of Leeds
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