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Abstract. Rifted margins form from extension and breakup of the con-tinental lithosphere. If this extension is coeval with a region of hotter litho-sphere, then it is generally assumed that a volcanic margin would follow. Here we present the results of numerical simulations of rift margin evolution...
Main Authors: | , , |
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Other Authors: | |
Format: | Text |
Language: | English |
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.655.6118 http://eprints.soton.ac.uk/66801/1/jjarmitage-submitted.pdf |