Structural peculiarities of phosphate minerals are discussed in correlation with the conditions of their crystallisation or transformation in the earth crust. Close structural relations in the row: lipscombite – barbosalite – trolleite – tavorite, are analyzed in order to unterstand the nature of paragenetic associations between these minerals or their analogues (Fe-trolleite).
Print ISSN: 0044-2968
Volume: 223, 01/2008
Pages: 126 - 131