SP503-2020-37_si_001.xlsx (176.74 kB)

Early to Middle Ordovician sedimentation and bimodal volcanism at the margin of Iapetus: The Trollhøtta–Kinna basin of the Central Norwegian Caledonides

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posted on 2021-02-12, 16:48 authored by Bjørgunn H. Dalsåen, Deta Gasser, Tor Grenne, Lars E. Augland, Arild Andresen

Analytical results for detrital zircon analyses.

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Geology not elsewhere classified

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detrital zircon analyses Iapetu Caledonides Analytical results Central Middle Ordovician sedimentation Trollh øtta basin bimodal volcanism Geology

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