Mantle convection for geologists
"Mantle convection is the fundamental agent driving many of the geological features observed at the Earth's surface, including plate tectonics and plume volcanism. Yet many Earth scientists have an incomplete understanding of the process. This book describes the physics and fluid dynamics...
I tiakina i:
| Kaituhi matua: | |
|---|---|
| Kaituhi rangatōpū: | |
| Hōputu: | Tāhiko īPukapuka |
| Reo: | Ingarihi |
| I whakaputaina: |
Cambridge ; New York :
Cambridge University Press,
2011.
|
| Ngā marau: | |
| Urunga tuihono: | An electronic book accessible through the World Wide Web; click to view |
| Ngā Tūtohu: |
Tāpirihia he Tūtohu
Kāore He Tūtohu, Me noho koe te mea tuatahi ki te tūtohu i tēnei pūkete!
|
Rārangi ihirangi:
- Machine generated contents note: 1. Introduction; 2. Context; 3. Why moving plates?; 4. Solid, yielding mantle; 5. Convection; 6. The plate mode of convection; 7. The plume mode of convection; 8. Perspective; 9. Evolution and tectonics; 10. Mantle chemical evolution; 11. Assimilating mantle convection into geology; Appendix A. Exponential growth and decay; Appendix B. Thermal evolution details; Appendix C. Chemical evolution details; References; Index.