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Fault-magma interactions during early continental rifting: Seismicity of the Magadi-Natron-Manyara basins, Africa
Although magmatism may occur during the earliest stages of continental rifting, its role in strain accommodation remains weakly constrained by largely 2D studies. We analyze seismicity data from a 13-month, 39-station broadband seismic array to determine the role of magma intrusion on state-of-stress and strain localization, and their along-strike variations.
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