Hawaiian volcanoes from source to surface
This monograph represents a sampling of the themes presented at the AGU Chapman Conference held in Waikoloa Beach on the Island of Hawaiʻi, August 20-24, 2012--
| Autor Corporativo: | |
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| Otros Autores: | , , , |
| Formato: | Libro electrónico |
| Idioma: | Inglés |
| Publicado: |
Washington, D.C. : Hoboken, NJ :
American Geophysical Union
[2015]
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| Colección: | Wiley ebooks.
Geophysical monograph series ; 208. |
| Acceso en línea: | Conectar con la versión electrónica |
| Ver en Universidad de Navarra: | https://innopac.unav.es/record=b46134347*spi |
Tabla de Contenidos:
- Title page; Table of Contents; Contributors; Preface; About the companion website; 1 How and Why Hawaiian Volcanism Has Become Pivotal to Our Understanding of Volcanoes from Their Source to the Surface; Abstract; 1.1. Introduction; 1.2. What Has Attracted Volcanologists to Hawai'i?; 1.3. How Have Studies of Hawaiian Volcanoes Influenced Our Knowledge of Magmatic and Volcanic Processes?; 1.4. Summary; Acknowledgments; References; 2 Seismic Constraints on a Double-Layered Asymmetric Whole-Mantle Plume Beneath Hawai'i; Abstract; 2.1. Introduction and Motivation; 2.2. Data and Method.
- 2.3. Imaging Results2.4. Resolution; 2.5. Discussion; 2.6. Summary; Acknowledgments; References; 3 Asymmetric Dynamical Behavior of Thermochemical Plumes and Implications for Hawaiian Lava Composition; Abstract; 3.1. Introduction; 3.2. Methods and Model Description; 3.3. Results; 3.4. Discussion; 3.5. Conclusions; Appendix: Melting, Density, and Rheology Parameterizations; Acknowledgments; References; 4 Major-Element and Isotopic Variations in Mauna Loa Magmas over 600 ka: Implications for Magma Generation and Source Lithology as Mauna Loa Transits the Hawaiian Plume; Abstract.
- 4.1. Introduction4.2. Compositional Variation in Mauna Loa Lavas; 4.3. Discussion; 4.4. Conclusions; Supplementary Digital Data; Acknowledgments; References; 5 Lithium Isotopic Signature of Hawaiian Basalts; Abstract; 5.1. Introduction; 5.2. Samples and Methods; 5.3. Results; 5.4. Discussion; 5.5. Conclusion; Supplementary Digital Data; Acknowledgments; References; 6 Onset of Rejuvenated-Stage Volcanism and the Formation of Līhu'e Basin: Kaua'i Events That Occurred 3-4 Million Years Ago; Abstract; 6.1. Introduction; 6.2. Setting; 6.3. Ages.
- 6.4. Geochemistry as Guide to Stratigraphic Assignment6.5. Age Range of Kōloa Volcanics; 6.6. Rates of Kōloa Stratigraphic Accumulation, Timing of Līhu'e Basin Formation, and Rates of Island Subsidence; 6.7. How Did the Līhu'e Basin Form?; 6.8. Summary; Acknowledgments; Appendix: Sample Descriptions; References; 7 Evidence for Large Compositional Ranges in Coeval Melts: Erupted from Kīlauea's Summit Reservoir; Abstract; 7.1. Introduction; 7.2. Context and Definitions; 7.3. Glass Compositions at Kīlauea Erupted During the Twentieth Century.
- 7.4. Discussion of Results for Twentieth-Century Eruptions7.5. Composition of Glasses in Older Kīlauea Tephra; 7.6. Discussion of Results for Tephra Glass Compositions; 7.7. Temporal and Spatial Constraints on Melt and Mineral Compositions in the Summit Reservoir; 7.8. Summary; 7.9. Conclusions; Supplementary Digital Data; Acknowledgments; References; 8 Petrologic Testament to Changes in Shallow Magma Storage and Transport During 30+ Years of Recharge and Eruption at Kīlauea Volcano, Hawai'i; Abstract; 8.1. Introduction; 8.2. Kīlauea Eruption Samples and Petrologic Data Sources.
