Geophysical characterisation of the ocean-continent transition at magma-poor rifted margins
Geophysical characterisation of the ocean-continent transition (OCT) at magma-poor rifted margins has focused primarily on the determination of P wave velocities using wide-angle seismic techniques. Such experiments have shown that the OCT is heterogeneous, but that typically velocities increase gra...
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| Format: | Article |
| Language: | English |
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2009-05.
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| Online Access: | Get fulltext |