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Detailed Reference Information |
Kanzaki, M., Stebbins, J.F. and Xue, X. (1991). Characterization of quenched high pressure phases in CaSiO3 system by XRD and 29Si NMR. Geophysical Research Letters 18: doi: 10.1029/91GL00463. issn: 0094-8276. |
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We have studied quenched high pressure phases in the CaSiO3 system by x-ray diffraction (XRD) and 29Si MAS NMR. XRD study of the previously reported ''&egr;-CaSiO3 phase'' synthesized at 12 GPa and 1500 ¿C reveals that it is actually a mixture of &bgr;-Ca2SiO4 (larnite) and a previously unknown CaSi2O5 phase. This result is supported by the 29Si NMR spectra. Furthermore, both the XRD and the NMR data suggest that the CaSi2O5 phase may have a titanite (CaTiSiO5) structure in which Ti is replaced by an octahedral Si. Samples quenched from 15 GPa and 1500 ¿C consist mostly of an amorphous phase, but a small amount of CaSiO3-perovskite was identified by both XRD and NMR. The 29Si NMR spectrum of the amorphous phase suggests that its local structure is similar to that of a glass quenched from melt at 1 bar. ¿ American Geophysical Union 1991 |
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BACKGROUND DATA FILES |
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Abstract |
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Keywords
Mineral Physics, High-pressure behavior, Mineral Physics, NMR, Mossbauer effects, and other magnetic properties, Mineral Physics, X ray, neutron, and electron spectroscopy and diffraction, Mineralogy, Petrology, and Rock Chemistry, Experimental mineralogy and petrology |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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