Refined estimates of the depths of magma chambers beneath the Reykjanes and Kolbeinsey Ridges, and implications for the structure of oceanic crust
The mid-Atlantic ridge is the divergent plate boundary between North and South America to the west and Europe and Africa to the east. Plate separation is accompanied by intrusion of dikes and eruption of lava along the ridge axis. The dikes are fed by magma chamber(s) located beneath the ridge and i...
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Format: | Thesis |
Language: | English |
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The Ohio State University
2009
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Online Access: | http://hdl.handle.net/1811/57010 |