Original language | English |
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Pages (from-to) | 173-187 |
Journal | Tectonophysics |
Volume | 410 |
DOIs | |
Publication status | Published - 2005 |
Middle to late Pleistocene uplift rate of the Hungarian Mountain Range at the Danube Bend, (Pannonian Basin) using in situ produced 3He
Z. Ruszkiczay-Rudiger, T.J. Dunai, G. Bada, L. Fodor, E. Horváth
Research output: Contribution to Journal › Article › Academic › peer-review