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Middle to late Pleistocene uplift rate of the Hungarian Mountain Range at the Danube Bend, (Pannonian Basin) using in situ produced 3He
Zs. Ruszkiczay-Rüdiger, T.J. Dunai, G. Bada, L. Fodor, E. HorváthVolume:
410
Year:
2005
Language:
english
DOI:
10.1016/j.tecto.2005.02.017
File:
PDF, 869 KB
english, 2005