Dynamic models for mantle flow and seismic anisotropy in the North Atlantic region and comparison with observations
[1] Dynamic mantle flow and temperature models for the North Atlantic based on a regionalized P-wave and a global S-wave tomography model were derived under the constraint of a maximum fit to the observed gravity field. For the regional flow model Cartesian geometry, temperature- and depth-dependent...
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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.459.1372 http://195.113.28.130/~oc/ggg07.pdf |