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A sedimentary basin that develops adjacent to an orogenic belt (orogen). subsidence is caused by loading of the crust through the stacking up of sheets of rock bounded by thrust faults in a foldthrust belt, the erosion of which supplies sediment to the basin. The migrating locus of deformation as shortening continues may result in the deformation of earlier foreland basins. Foreland basins contain an important record of the growth of major mountain chains. Presentday examples include the molasse basin of the Alps and the Ganges basin south of the Himalayas.

GeraintOwenSwansea University
10.4135/9781446247501.n1534

AllenPA and AllenJR (2004) Basin analysis: Principles and applications. Chichester: Wiley.
CorrochanoD, BarbaP and ColmeneroJR (2012) Glacioeustatic cyclicity of a Pennsylvanian carbonate platform in a foreland basin setting: An example from the Bachende Formation of the Cantabrian Zone (NW Spain). Sedimentary Geology245: 7693.
DeCelles, PG (2004) Late Jurassic to Eocene evolution of the Cordilleran thrust belt and foreland basin system, western USA. American Journal of Science304: 105168.
EvansMJ and ElliottT (1999) Evolution of a thrust-sheet-top basin: The Tertiary Barreme basin, Alpes-de-Haute-Provence, France. Bulletin of the Geological Society of America111: 16171643.
GuptaS (1997) Himalayan drainage patterns and the origin of fluvial megafans in the Ganges foreland basin. Geology25: 1114.
Najman, Y. (2006) The detrital record of orogenesis: A review of approaches and techniques used in the Himalayan sedimentary basins. Earth-Science Reviews74: 172.
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