Dissolution of orthopyroxene in basanitic magma between 0.4 and 2 GPa: further implications for the origin of Si-rich alkaline glass inclusions in mantle xenoliths

Artigo Revisado por pares

1999; Springer Science+Business Media; Volume: 135; Issue: 2-3 Linguagem: Inglês

10.1007/s004100050501

ISSN

1432-0967

Autores

Cliff S. J. Shaw,

Tópico(s)

earthquake and tectonic studies

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