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 JournalArticleAcademicpeer-review

    Original languageEnglish
    Pages (from-to)173-187
    JournalTectonophysics
    Volume410
    DOIs
    Publication statusPublished - 2005

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