Index: Chapter 1. Composition of the Earth and implication for geodynamics William F. McDonough Chapter 2. Plumes from the heterogeneous Earth’s mantle Cinzia G. Farnetani Chapter 3. Nature and origin of heterogeneities in the lithospheric mantle in the context of asthenospheric upwelling and mantle wedge zones: What do mantle xenoliths tell us? M. Grégoire, G. Delpech, B. Moine and J.-Y. Cottin Chapter 4. Simple models for trace element fractionation during decompression melting of a two-lithology mantle Yan Liang Chapter 5. The shallow mantle as a reactive filter: a hypothesis inspired and supported by field observations Georges Ceuleneer, Mathieu Rospabé, Michel Grégoire and Mathieu Benoit Chapter 6. The role of H2O in the deformation and microstructural evolution of the upper mantle Károly Hidas and José Alberto Padrón-Navarta Chapter 7. Kinetic controls on the thermometry of mantle rocks: A case study from the Xigaze Ophiolites, Tibet L. Zhao and S. Chakraborty
Chemical Geodynamics of Earth's Mantle: New Paradigms
C. Bonadiman
Primo
;
2024
Abstract
Index: Chapter 1. Composition of the Earth and implication for geodynamics William F. McDonough Chapter 2. Plumes from the heterogeneous Earth’s mantle Cinzia G. Farnetani Chapter 3. Nature and origin of heterogeneities in the lithospheric mantle in the context of asthenospheric upwelling and mantle wedge zones: What do mantle xenoliths tell us? M. Grégoire, G. Delpech, B. Moine and J.-Y. Cottin Chapter 4. Simple models for trace element fractionation during decompression melting of a two-lithology mantle Yan Liang Chapter 5. The shallow mantle as a reactive filter: a hypothesis inspired and supported by field observations Georges Ceuleneer, Mathieu Rospabé, Michel Grégoire and Mathieu Benoit Chapter 6. The role of H2O in the deformation and microstructural evolution of the upper mantle Károly Hidas and José Alberto Padrón-Navarta Chapter 7. Kinetic controls on the thermometry of mantle rocks: A case study from the Xigaze Ophiolites, Tibet L. Zhao and S. ChakrabortyI documenti in SFERA sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
