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You are here: Home / Geology / bibliografie geology / biblio geology Belgium / biblio nw 17000 - 17999 / Long-term river terrace sequences: Evidence for global increases in surface uplift rates in the Late Pliocene and early Middle Pleistocene caused by flow in the lower continental crust induced by surface processes

R Westaway (2002)

Long-term river terrace sequences: Evidence for global increases in surface uplift rates in the Late Pliocene and early Middle Pleistocene caused by flow in the lower continental crust induced by surface processes

Netherlands Journal of Geosciences / Geologie en Mijnbouw, vol. 81 p. 305-328.

17940, .94, ALL, PLEIS, NEOTEC, RIV

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