Artigo Revisado por pares

Segregation and cation-ordering in sjögrenite and pyroaurite

1969; Cambridge University Press; Volume: 37; Issue: 287 Linguagem: Inglês

10.1180/minmag.1969.037.287.04

ISSN

1471-8022

Autores

H. F. W. Taylor,

Tópico(s)

Methane Hydrates and Related Phenomena

Resumo

Summary A specimen from Långban, Sweden, was found to consist largely of sjögrenite in which segregation and ordering of the metal cations had occurred, yielding an intergrowth of regions of two main types with compositions probably of or near Mg 2/3 Fe 1/3 (OH) 2 (CO 3 ) 1/6 (H 2 O) 0·4 and Mg 12/13 Fe 1/13 (OH) 2 (CO 3 ) 1/26 (H 2 O) 0·8 . To a smaller extent segregation had proceeded further, giving regions probably approximating to the end-member Mg(OH) 2 .H 2 O. It is suggested that the names sjögrenite and pyroaurite be used for the 2H- and 3R- polytypes of this structure irrespective of Mg:Fe ratio, segregation, or cation ordering.

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