Seismic anisotropy in the deep mantle could partly be derived from the deformation of hydrous phase D
Phase D, an elastically anisotropic hydrous mineral ... on phase D aggregates under conditions of the lower mantle transition ...
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Seismic anisotropy in the deep mantle could partly be derived from the deformation of hydrous phase D
(a, b) Images show deformation cell assemblage and microstructure of shear-deformed Al bearing-phase D aggregate under 20GPa, 800°C, conditions of lower mantle transition zone. Large deviation of ...
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Microstructure and CPO of shear-deformed Al bearing-phase D. (IMAGE)
(a, b) Images show deformation cell assemblage and microstructure of shear-deformed Al bearing-phase D aggregate under 20GPa, 800°C, conditions of lower mantle transition zone. Large deviation of ...