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Metasomatism and the Chemical Transformation of Rock The Role of Fluids in Terrestrial and Extraterrestrial Processes /
Fluid-aided mass transfer and subsequent mineral re-equilibration are the two defining features of metasomatism and must be present in order for metamorphism to occur. Coupled with igneous and tectonic processes, metasomatism has played a major role in the formation of the Earth's continental a...
| Clasificación: | Libro Electrónico |
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| Autores principales: | , |
| Autor Corporativo: | |
| Formato: | Electrónico eBook |
| Idioma: | Inglés |
| Publicado: |
Berlin, Heidelberg :
Springer Berlin Heidelberg : Imprint: Springer,
2013.
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| Edición: | 1st ed. 2013. |
| Colección: | Lecture Notes in Earth System Sciences,
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| Temas: | |
| Acceso en línea: | Texto Completo |
Tabla de Contenidos:
- 1. Metasomatism and the chemical transformation of rock: Rock-mineral-fluid interaction in terrestrial and extraterrestrial environments. -2. The Chemical Composition of Metasomatic Fluids in the Crust
- 3. Thermodynamic modeling and thermobarometry of metasomatized rocks
- 4. Structural controls of metasomatism on a regional scale
- 5. Mechanisms of metasomatism and metamorphism on the local mineral scale: The role of dissolution-reprecipitation during mineral re-equilibration. - 6. Geochronology of metasomatic events.-7. Effects of metasomatism on mineral systems and their host rocks: alkali metasomatism, skarns, greisens, tourmalinites, rodingites, black-wall alteration and listevenites
- 8. Metasomatism within the ocean crust
- 9. Metasomatism in subduction zones of subducted oceanic slabs, mantle wedges, and the slab-mantle interface
- 10. Metasomatism during High-Pressure Metamorphism: Eclogites and Blueschist-Facies Rocks
- 11. Prograde, peak and retrograde metamorphic fluids and associated metasomatism in upper amphibolite to granulite facies transition zones
- 12. Mantle Metasomatism
- 13. Mapping the distribution of fluids in the crust and lithospheric mantle utilizing geophysical methods
- 14. A Hydromechanical Model for Lower Crustal Fluid Flow
- 15. Metasomatism in the early solar sysem: The record fron Chondritic meteorites.