Abstract
The crystal structure of a fibrous sussexite Mn1.91Mg0.09B2O4(OH)2 was solved and refined from single-crystal X-ray data collected on (001) twinned crystals. Sussexite is isotypic to szaibelyite (Mg)2B2O4(OH)2, both crystallizing in space group P21/c. Two non-equivalent chains of Mn/Mg octahedra (Mn1, Mn2) are connected by corners thus forming layers perpendicular to the c-axis. These sheets are linked by triangular pyroborate-groups [B2O4(OH)]3-. In addition, hydrogen bridges stabilize the octahedral layer structure. The cleavage plane of sussexite is parallel to the octahedral layers. The twinning of sussexite can not be resolved under the polarizing microscope; thus the twin components have either a very similar optic orientation or more probably, the twinning is on a submicroscopic scale. -from Authors
Original language | English |
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Pages (from-to) | 123-133 |
Number of pages | 11 |
Journal | Schweizerische Mineralogische und Petrographische Mitteilungen |
Volume | 75 |
Issue number | 1 |
State | Published - 1995 |
Externally published | Yes |