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The document summarizes the formation and evolution of the mid-Norwegian volcanic passive margins. It discusses: 1) The margins formed as a result of rifting and breakup of the North Atlantic Igneous Province in the Early Eocene. Massive intrusions of mafic rock occurred during this time. 2) The margins are characterized by seaward dipping lava flows, intrusion of dykes and sills into sediments, and underplating of the lower crust by mafic magma. 3) The margins developed over three segments through rif

Author

Sam

Language

EN