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Several copper anomalies were found near Langtjernet at the eastern end of Sandølafeltet during the regional stream sediment survey in 1973 (NGU oppdrag nr. 1177, Grongprosjektet, kartblad Andorsjøen 1823 I). This locality lies mostly within the Sandøla trondhjemite but includes the contact with a green- stoneunit. Some samples were subsequently analysed for molybdenum and several were found to be anomalous. This led G. Gale and R.
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