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The study investigates the selective metasomatism of ultramafic cumulates in the Neoarchean Storø Supracrustal Belt in SW Greenland, focusing on the occurrence of tourmaline orbicules within these rocks. It reveals that these orbicules formed from melts rich in boron and water, influenced by the silicification of ultramafic rocks, contributing to the geochemical diversity of Archean ultramafic rocks. The findings enhance the understanding of the early Earth

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