Abstract
The structure of preiswerkite, ideally Na(Mg2Al)(Si2Al2)O10(OH)2, from the type locality at Geisspfad in Switzerland, has been determined by single-crystal X-ray diffraction and refinement. The polytype is 1M with space group C2/m. The unit-cell parameters are a = 5.228(7), b = 9.049(10), c = 9.819(12) Å, β = 100.42(13)°. Preiswerkite shares specific structures properties with a number of micas with very different compositions; apart from tetrahedral ordering, the closest structural analogue seems to be ephesite, ideally Na(LiAl2)(Si2Al2)O10(OH)2, which differs chemically only by the octahedral substitution Mg + Mg ⇌ Li + Al. -from Authors
Original language | English |
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Pages (from-to) | 1290-1298 |
Number of pages | 9 |
Journal | American Mineralogist |
Volume | 78 |
Issue number | 11-12 |
State | Published - 1993 |
Externally published | Yes |