The Evolution of the Chilean-Argentinean Andes
This book describes the Mesozoic to Cenozoic evolution of the Chilean and Argentinean Andes. The book is structured from a historical perspective concentrating on specific processes explained in each chapter. The chapters cover dynamic subsidence; neotectonics; magmatism; long and short term deforma...
Gespeichert in:
| Format: | Elektronisch E-Book |
|---|---|
| Sprache: | Englisch |
| Veröffentlicht: |
Cham :
Springer International Publishing,
2018.
|
| Ausgabe: | 1st ed. 2018. |
| Schriftenreihe: | Springer Earth System Sciences,
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| Schlagworte: | |
| ISBN: | 9783319677743 |
| ISSN: | 2197-9596 |
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Inhaltsangabe:
- Preface.- 1.Crustal structure and tectonics of the Chilean continental margin from wide-angle seismic studies: a review
- 2. Crustal and thermal structure along the Chilean subduction margin from gravity data and their relation to short and long term segmentation: a review
- 3. The Peru-Chile margin revisited with global gravity field derivatives
- 4.The Pre-Andean phases of construction of the Southern Andes basement
- 5. The geometry of the subduction margin from paleomagnetic data: a review
- 6. The early stages of the volcanic arc in the Southern Andes
- 7. The early orogeny stages in the Southern Central and Patagonian Andes
- 8.The Mesozoic to Cenozoic structure and tectonic evolution of the Southern Patagonian Andes.-9. Andean and foreland Cenozoic sources during mountain growth evolution
- 10. The Cenozoic structure and tectonic evolution of the Southern Central Andes
- 11. The Cenozoic structure and tectonic evolution of the Northern Patagonian Andes
- 12. The origin of the Neogene transgressions during the Andean development
- 13. Landscape and tectonics of the Central Chilean Andes
- 14. Landscape and tectonics of the Northern Chilean Andes
- 15. The Neogene volcanic arc from the southern Altiplano to the Southern Central Andes.-16. Dynamic subsidence and uplift associated with the Pampean flat subduction zone
- 17.Thermal structure associated with the Pampean flat subduction zone
- 18. Architecture and evolution of the volcanic arc in the last 5 Ma along the Southern Central and Patagonian Andes
- 19.The late segmentation of the Southern Andes as a function of ocean bathymetry.

