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Forventes på lager: 23-08-2016
The Earth's rocky mantle convects to lose heat, which comes from the liquid iron core below. 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.
| Forlag | Springer-Verlag Berlin and Heidelberg GmbH & Co. KG |
| Forfatter | Andy Nowacki |
| Type | Bog |
| Format | Paperback / softback |
| Sprog | Engelsk |
| Udgave | Softcover reprint of the original 1st ed. 2013 |
| Udgivelsesdato | 23-08-2016 |
| Første udgivelsesår | 2016 |
| Serie | Springer Theses |
| Illustrationer | XVI, 166 p. |
| Originalsprog | Germany |
| Sideantal | 166 |
| Indbinding | Paperback / softback |
| Forlag | Springer-Verlag Berlin and Heidelberg GmbH & Co. KG |
| Sideoplysninger | 166 pages, XVI, 166 p. |
| Mål | 235 x 155 |
| ISBN-13 / EAN-13 | 9783662510995 |