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Som del af en verdensturné gæster Douglas Oldenburg Institut for Geoscience med dette kursus i to dage.
Sequence stratigraphy of the Cenozoic in the Central North Sea
Equilibrium theory, evolution and least action principle; factors determining self-adjustment in geomorphology and Earth’s fluvial stratigraphic…
Late accretion history of the terrestrial planets from highly siderophile elements and their isotopes
Hvad kan Fe-isotoper fortælle os om magmaer?
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