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Researchers from the Department of Earth Science of the University of Bergen explain in a paper published in Nature Communications how exhumed mantle domes form at magma-poor continental margins and at ultra-slow mid-oceanic spreading systems controlled b
New article in Nature Communications (31.03.2022)
Researchers from the Department of Earth Science of the University of Bergen explain in a paper published in Nature Communications how exhumed mantle domes form at magma-poor continental margins and at ultra-slow mid-oceanic spreading systems controlled by frictional shear zones.