High-pressure Al-rich hexagonal phases-What are their kin?

Emil Makovicky; Lars Arnskov Olsen

doi:10.2138/am.2008.2859

High-pressure Al-rich hexagonal phases-What are their kin?

1 Citationer (Scopus)

Abstract

The hexagonal Al-rich high-pressure phases are members of a structural family with the same type of framework composed of double-ribbons of edge-sharing octahedra, but variably occupied trigonal and hexagonal channels. This family includes jaffeite, fluoborite, yeremeyevite, painite, and synthetic Ba indates. This kinship broadens the spectrum of elements potentially accommodated by these phases in the mantle.

Originalsprog	Engelsk
Tidsskrift	American Mineralogist
Vol/bind	93
Udgave nummer	10
Sider (fra-til)	1585-1587
ISSN	0003-004X
DOI	https://doi.org/10.2138/am.2008.2859
Status	Udgivet - 2008

Emneord

Det Natur- og Biovidenskabelige Fakultet
krystal strukturer

Adgang til dokumentet

10.2138/am.2008.2859

Citationsformater

@article{89aedc70bf9a11dd8e02000ea68e967b,

title = "High-pressure Al-rich hexagonal phases-What are their kin?",

abstract = "The hexagonal Al-rich high-pressure phases are members of a structural family with the same type of framework composed of double-ribbons of edge-sharing octahedra, but variably occupied trigonal and hexagonal channels. This family includes jaffeite, fluoborite, yeremeyevite, painite, and synthetic Ba indates. This kinship broadens the spectrum of elements potentially accommodated by these phases in the mantle.",

keywords = "Faculty of Science, krystal strukturer, Al-rich high-pressure phases, framework of octahedra, painite, fluoborite, jaffeite, crystal structure, Jeremejevite, Painite",

author = "Emil Makovicky and Olsen, {Lars Arnskov}",

year = "2008",

doi = "10.2138/am.2008.2859",

language = "English",

volume = "93",

pages = "1585--1587",

journal = "American Mineralogist",

issn = "0003-004X",