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Volcanic Rifted Margins
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Non-volcanic Rifting of Continental Margins
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Non-continental margins lack thick lavas that are generated as continental crust thins immediately prior to the onset of seafloor spreading. They may form up to
Magmatic Rifting and Active Volcanism
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A major rifting episode began in the Afar region of northern Ethiopia in September 2005. Over a ten-day period, c. 2.5 km3 of magma were intruded along a 60 km-
Evolution of Volcanic Rifted Margins
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Evolution of Volcanic Rifted Margins
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