Abstract
The substitution NaNa□-1Ca-1, which fills the A site, has been investigated in amphiboles close to the join tremolite-richterite. At 1123 K, compositions of amphiboles synthesized from bulk compositions on this binary are displaced towards magnesio-cummingtonite [Mg7Si8O22(OH)2], such that average compositions are better represented by the pseudobinary tremolite92magnesio-cummingtonite8-richterite. Major-element compositions and H2O contents are close to theoretical values for eight samples synthesized along this join. Unit-cell parameters vary smoothly with composition, a sin β showing the greatest increase as Na fills the A site. High-resolution transmission electron microscopy demonstrates that the amphiboles are highly ordered, with only the tremolite-rich compositions containing any chain multiplicity faults. -from Authors
Original language | English |
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Pages (from-to) | 23-35 |
Number of pages | 13 |
Journal | American Mineralogist |
Volume | 78 |
Issue number | 1-2 |
Publication status | Published - 1 Jan 1993 |
Keywords
- amphibole
- mineral synthesis
- richterite
- thermochemistry
- tremolite