Redefinition of angastonite, CaMgAl<sub>2</sub>(PO<sub>4</sub>)<sub>2</sub>(OH)<sub>4</sub> ⋅ 7H<sub>2</sub>O, as an amorphous mineral
Abstract 2 (PO4) 2 4 ⋅ 7 H2 O, has been found to correspond to the amorphous phase. A proposal for the redefinition of angastonite as an amorphous phase has been approved by the IMA CNMNC. Amorphous angastonite is isotropic with an index of refraction in the range 1.33 to 1.40 and a measured density of 1.57 (2) g cm- 3. It is formed from incongruent leaching of minyulite in circulating Mg- and Ca-bearing solutions. The amorphous phase undergoes local recrystallisation to form penriceite and two other new crandallite-derivative layer phases. A cluster model for the local structure in the amorphous mineral is proposed based on crandallite-type segments. A brief review of amorphous minerals is given.
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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Redefinition of angastonite, CaMgAl2(PO4)2(OH)4 ⋅ 7H2O, as an amorphous mineral ; volume:34 ; number:2 ; year:2022 ; pages:215-221 ; extent:7
European journal of mineralogy ; 34, Heft 2 (2022), 215-221 (gesamt 7)
- Creator
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Grey, Ian Edward
Elliott, Peter
Mumme, William Gus
MacRae, Colin M.
Kampf, Anthony R.
Mills, Stuart J.
- DOI
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10.5194/ejm-34-215-2022
- URN
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urn:nbn:de:101:1-2022041405295698991321
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
- 15.08.2025, 7:32 AM CEST
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Associated
- Grey, Ian Edward
- Elliott, Peter
- Mumme, William Gus
- MacRae, Colin M.
- Kampf, Anthony R.
- Mills, Stuart J.
Other Objects (12)
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