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Volcanic and Igneous Plumbing Systems : Understanding Magma Transport, Storage, and Evolution in the Earth's Crust /
"Volcanic and Igneous Plumbing Systems: Understanding Magma Transport, Storage, and Evolution in the Earth's Crust synthesizes research from various geoscience disciplines to examine volcanic and igneous plumbing systems (VIPS) in-depth. VIPS comprise a network of magma transport and stora...
| Clasificación: | Libro Electrónico |
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| Otros Autores: | |
| Formato: | Electrónico eBook |
| Idioma: | Inglés |
| Publicado: |
Amsterdam, Netherlands :
Elsevier,
[2018]
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| Temas: | |
| Acceso en línea: | Texto completo |
Tabla de Contenidos:
- Intro; Title page; Table of Contents; Copyright; List of Contributors; Chapter 1: Introduction to Volcanic and Igneous Plumbing Systems-Developing a Discipline and Common Concepts; Abstract; 1.1. Introduction; 1.2. Developing A Scientific Discipline; 1.3. The History of Research on Magmatic Systems; 1.4. Conflicting Perspectives: Of Balloons, Blobs and Mush; 1.5. Overview of Contributions in This Book; 1.6. Concluding Remarks; Chapter 2: Mechanisms of Magma Transport and Storage in the Lower and Middle Crust-Magma Segregation, Ascent and Emplacement; Abstract; 2.1. Introduction.
- 2.2. Production and Removal of Magmas from Migmatitic Sources2.3. Magma Ascent Mechanisms; 2.4. Growth and Emplacement of Mid-Crustal Magma Reservoirs; 2.5. Concluding Remarks; Chapter 3: Mechanisms of Magma Transport in the Upper Crust-Dyking; Abstract; 3.1. Introduction; 3.2. Methods to Study Dyke Propagation; 3.3. Dyke Geometry; 3.4. Host-Rock Deformation; 3.5. Impact of Stress and Crustal Heterogeneity; 3.6. Magma Flow; 3.7. Feeder and Non-Feeder Dykes; 3.8. Summary and Future Opportunities; Field Example: The Swartruggens Kimberlite Dyke Swarm, South Africa; Acknowledgements.
- Chapter 4: Growth of a Volcanic Edifice Through Plumbing System Processes-Volcanic Rift Zones, Magmatic Sheet-Intrusion Swarms and Long-Lived ConduitsAbstract; 4.1. Introduction; 4.2. Volcanic Rift Zones and Their Intrusion Swarms; 4.3. Cone-Sheet Swarms; 4.4. Radial Dyke Swarms; 4.5. Why Do Different Types of Sheet Intrusions Occur in the Same Volcano?; 4.6. Volcanic Conduits; 4.7. Summary; Field Example: Intrusive Sheet Swarms in the Canary Islands; Field Example: Exposed Conduits in Central Iceland.
- Chapter 5: Storage and Transport of Magma in the Layered Crust-Formation of Sills and Related Flat-Lying IntrusionsAbstract; 5.1. Introduction; 5.2. What are Sills? Definitions and Morphologies; 5.3. Where do Sills Occur?; 5.4. How do Sills Form?; 5.5. Scientific and Economic Relevance of Sills; 5.6. Summary; Field Example: The Golden Valley Sill Complex, Karoo Basin, South Africa; Chapter 6: Pascal's Principle, a Simple Model to Explain the Emplacement of Laccoliths and Some Mid-crustal Plutons; Abstract; 6.1. Introduction.
- 6.2. How Do Laccoliths and Other Large Magma Bodies Grow From Sills? Examples From the Henry Mountains6.3. Conceptual Model for the Growth of Laccoliths From Sills; 6.4. Pascal's Principle Applied to the Emplacement of Mid-Crustal Intrusions; 6.5. Conclusions; Acknowledgements; Chapter 7: Tectonics and Volcanic and Igneous Plumbing Systems; Abstract; 7.1. Introduction; 7.2. How is Magma Transported and Stored in Divergent Geodynamic Settings?; 7.3. In Mantle Plumes How is Magma Stored and Transported?; 7.4. How is Magma Transported and Stored in Convergent Geodynamic Settings?