High-pressure single-crystal X-ray diffraction and infrared spectroscopic studies of the C2/m-P21/m phase transition in cummingtonite
The structural changes associated with the C2/m-P21/m phase transition in cummingtonite with (Fe+Mn)/(Fe+Mn+Mg)≈0.50 have been studied with single-crystal X-ray diffraction at various pressures up to 7.90 GPa and infrared spectroscopy up to 8.63 GPa. With increasing pressure, the crystal transforms...
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Veröffentlicht in: | The American mineralogist 1998-03, Vol.83 (3-4), p.288-299 |
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