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Showing 1 to 1 of 1 for “"Magma-poor continental rifting"”.
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Investigating the Kinematics and Dynamics of Strain Localization in the Northern Western Branch of the East African Rift System
Continental rifts are thought to be formed by repeated episodes of magmatism, reactivation of pre-existing structures, or a combination of both. Continental rifts are evidence of a divergent plate boundary, where tectonic plates are breaking apart. The northern Western Branch of the East African …