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Mineralogical effects on the detectability of the postperovskite boundary
The discovery of a phase transition in Mg-silicate perovskite (Pv) to postperovskite (pPv) at lowermost mantle pressure-temperature (P - T) conditions may provide an explanation for the discontinuous increase in shear wave velocity found in some regions at a depth range of 200 to 400 km above the co...
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Main Authors: | , , , |
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Formato: | Artigo |
Idioma: | Inglês |
Publicado em: |
National Academy of Sciences
2012
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Assuntos: | |
Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3289301/ https://ncbi.nlm.nih.gov/pubmed/22308329 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1109204109 |
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