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The Svecofennian Orogen is a geological formation in the Baltic Shield, extending through northern Sweden, southern Finland, and western Russia. It formed between 1.9 and 1.7 billion years ago. This orogenic belt is characterized by a suture zone containing ophiolite complexes, which are remnants of oceanic crust. Copper mineralization is found within these oceanic crust rocks. To the north of the suture lies a shelf-type sedimentary sequence, while a volcanic-plutonic arc is present to the south. Further south, a zone of thrusted gneisses intruded by tin-bearing granites, known as rapakivi granites, likely formed due to mantle plume activity. The Svecofennian Orogen is part of the Precambrian geology of Europe.12

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