Mineralogical Journal
Online ISSN : 1881-4174
Print ISSN : 0544-2540
ISSN-L : 0544-2540
Volume 8, Issue 4
Displaying 1-5 of 5 articles from this issue
 
  • Sakichi ASHIDA, Yukio ITO
    1976Volume 8Issue 4 Pages 215-225
    Published: 1976
    Released on J-STAGE: March 31, 2007
    JOURNAL FREE ACCESS
    Neodymium pentaphosphate (NdP5O14) crystals are grown by the flux method. The crystals obtained are 3 to 7 mm in diameter and 1 to 3 mm in thickness.
    Lattice parameters are a0=13.012±0.008Å, b0=8.967±0.006Å, c0=8.756±0.005Å, β=90.56±0.02° and the space group is P21a. The orientation of the optic elastic axes referred to the crystal axes for D(5893Å) line is as follows; Y∧c=8.2°, X=b, Z∧a=7.7°, 2V=(+)64.0±2°. Refractive indices for D-line are α=1.609, β=1.613, γ=1.629. Twin planes (100) and (001) are observed in NdP5O14 under the polarizing microscope between crossed nicols. The twin boundaries migrate by an external stress along the [-101] and [10-1] directions.
    When the temperature is raised, they disappear at 149±1°C and the extinction angle (c∧Y) becomes 0°. This phase transition is of the thermodynamically second order. According to the Aizu theory, NdP5O14 crystals belong to the mmm1′F2⁄m1′ species.
    Download PDF (1056K)
  • Eiji OHTANI, Hiroshi SAWAMOTO
    1976Volume 8Issue 4 Pages 226-233
    Published: 1976
    Released on J-STAGE: March 31, 2007
    JOURNAL FREE ACCESS
    The phase relation in the pseudobinary system Fe2SiO4–FeAl2O4 has been studied under the conditions up to 100 kbar and to 1300°C. The reaction of Fe2SiO4 (fayalite) and FeAl2O4 (hercynite) to Fe3Al2Si3O12 (almandine) and FeO (wustite) was clarified to occur above 25 kbar at 1000°C.
    Preliminary experiments in the system Co2SiO4–CoAl2O4 have also been performed and a similar reaction, 3Co2SiO4+CoAl2O44CoO+Co3Al2Si3O12, was found to occur.
    It is suggested that another similar reaction, 3Mg2SiO4+MgAl2O44MgO+Mg3Al2Si3O12, may occur in the system Mg2SiO4–MgAl2O4 and that there is no possibility of complete solid solubility between aluminate spinel and silicate spinel.
    Download PDF (475K)
Short Communications
feedback
Top