High-pressure Al-rich hexagonal phases-What are their kin?
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High-pressure Al-rich hexagonal phases-What are their kin? / Makovicky, Emil; Olsen, Lars Arnskov.
I: American Mineralogist, Bind 93, Nr. 10, 2008, s. 1585-1587.Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt
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TY - JOUR
T1 - High-pressure Al-rich hexagonal phases-What are their kin?
AU - Makovicky, Emil
AU - Olsen, Lars Arnskov
PY - 2008
Y1 - 2008
N2 - 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.
AB - 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.
KW - Faculty of Science
KW - krystal strukturer
KW - Al-rich high-pressure phases
KW - framework of octahedra
KW - painite
KW - fluoborite
KW - jaffeite
KW - crystal structure
KW - Jeremejevite
KW - Painite
U2 - 10.2138/am.2008.2859
DO - 10.2138/am.2008.2859
M3 - Journal article
VL - 93
SP - 1585
EP - 1587
JO - American Mineralogist
JF - American Mineralogist
SN - 0003-004X
IS - 10
ER -
ID: 8804849