Microstructures and seismic properties of south Patagonian mantle xenoliths (Gobernador Gregores and Pali Aike)

The subcontinental lithospheric mantle evolves through time due to tectonic events and processes as static recrystallization and melt percolation. To constrain the extent of these processes in the South Patagonian subcontinental mantle lithosphere we performed a microstructural and Electron Backscat...

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Detalles Bibliográficos
Autores principales: Zaffarana, C., Tommasi, A., Vauchez, A., Grégoire, M.
Formato: JOUR
Materias:
Annealing
Crystal preferred orientations
Melt percolation
Olivine
Orthopyroxene
Subcontinental mantle lithosphere
Birefringence
Deformation
Lithology
Seismology
Shear waves
Solvents
Tectonics
Wave propagation
Crystallographic preferred orientations
Electron back-scattered diffraction
Melt percolations
Static recrystallization
Sub-continental lithospheric mantles
Subcontinental mantle
Structural geology
annealing
continental lithosphere
crystallography
deformation
mantle structure
olivine
orientation
orthopyroxene
P-wave
S-wave
seismology
tectonic evolution
volcanic rock
wave propagation
xenolith
Argentina
Gobernador Gregores
Pali Aike Volcanic Field
Santa Cruz [Argentina]
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00401951_v621_n_p175_Zaffarana
Aporte de:
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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