Plate Deformation from Cradle to Grave Seismic Anisotropy and Deformation at Mid-Ocean Ridges and in the Lowermost Mantle /
The mantle’s interfaces – the core-mantle boundary and the lithosphere – may hold the key to understanding mantle motion, because of the seismic anisotropy present in these parts of the Earth. This thesis contains a substantive introduction to the structure of the Earth, seismic anisotropy in the...
| Κύριος συγγραφέας: | |
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| Συγγραφή απο Οργανισμό/Αρχή: | |
| Μορφή: | Ηλεκτρονική πηγή Ηλ. βιβλίο |
| Γλώσσα: | English |
| Έκδοση: |
Berlin, Heidelberg :
Springer Berlin Heidelberg : Imprint: Springer,
2013.
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| Σειρά: | Springer Theses, Recognizing Outstanding Ph.D. Research,
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| Θέματα: | |
| Διαθέσιμο Online: | Full Text via HEAL-Link |
Πίνακας περιεχομένων:
- Seismic anisotropy and deformation in the lowermost mantle
- Mantle anisotropy beneath the Earth’s mid-ocean ridges
- Deformation of the lowermost mantle from seismic anisotropy
- Predicting lowermost mantle anisotropy using models of mantle flow.
