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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

✍ Scribed by Zs. Ruszkiczay-Rüdiger; T.J. Dunai; G. Bada; L. Fodor; E. Horváth


Book ID
116908150
Publisher
Elsevier Science
Year
2005
Tongue
English
Weight
869 KB
Volume
410
Category
Article
ISSN
0040-1951

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