The crystal structure of vlodavetsite, AlCa2(SO4)2F2Cl.4H2O, has been determined. The polyhedron cation chains are parallel to [001] and consist of couples of distorted Ca octahedra alternating with one distorted Al octahedron rotated through 24° with respect to the former. The chains are linked by SO4-tetrahedra so that all of the four tetrahedron oxygen atoms take part in coordination of Ca atoms to form a distorted octahedron with Cl and F atoms. The Al coordination polyhdron consists of two F atoms and four oxygen atoms belonging to water molecules. There is a specific interaction via hydrogen bonds between oxygen atoms of SO4-tetrahedra and water molecules. -from Authors

Язык оригиналаанглийский
Страницы (с-по)159-162
Число страниц4
ЖурналMineralogical Magazine
Том59
Номер выпуска1
СостояниеОпубликовано - 1 янв 1995

    Предметные области Scopus

  • Геохимия и петрология

ID: 53955949