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

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Standard

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

Harvard

Makovicky, E & Olsen, LA 2008, 'High-pressure Al-rich hexagonal phases-What are their kin?', American Mineralogist, bind 93, nr. 10, s. 1585-1587. https://doi.org/10.2138/am.2008.2859

APA

Makovicky, E., & Olsen, L. A. (2008). High-pressure Al-rich hexagonal phases-What are their kin? American Mineralogist, 93(10), 1585-1587. https://doi.org/10.2138/am.2008.2859

Vancouver

Makovicky E, Olsen LA. High-pressure Al-rich hexagonal phases-What are their kin? American Mineralogist. 2008;93(10):1585-1587. https://doi.org/10.2138/am.2008.2859

Author

Makovicky, Emil ; Olsen, Lars Arnskov. / High-pressure Al-rich hexagonal phases-What are their kin?. I: American Mineralogist. 2008 ; Bind 93, Nr. 10. s. 1585-1587.

Bibtex

@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",
publisher = "Mineralogical Society of America",
number = "10",

}

RIS

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