Modelling the composition of melts formed during continental breakup of the Southeast Greenland margin
We have developed a generic dynamic model of extension of the lithosphere, which predicts major element composition and volume of melt generated from initial extension to steady state seafloor spreading. Stokes equations for non-Newtonian flow are solved and the mantle melts by decompression. Streng...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
2008-05-15.
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| Subjects: | |
| Online Access: | Get fulltext |