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1. REE mineralisation and metasomatic alteration in the Olserum metasediments
University essay from Lunds universitet/Geologiska institutionenAbstract : The Olserum mineralisation is situated in the metasediments of the Västervik formation, which repre-sents the southernmost continental margin of the Svecokarelian Domain. After deposition between 1.88 – 1.85 Ga these sediments were subsided to a depth of about 10 km and intruded by a series of granitoid melts. READ MORE
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