NJG50-1-02
1970
The occurrence of olivine hyperite at Ødegårdens verk, Bamble, South Norway
50
1
15-17

A study of the first find of olivine relics in hyperite at Ødegårdens Verk and the surrounding coronas leads to the conclusion that the second rim of garnet is of metamorphic origin while a third rim of scapolite is apparently related to a later magmatic phase.

0029-196X
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