High-pressure behaviour of germanate olivines studied by X-ray diffraction and X-ray absorption spectroscopy

Physics and Chemistry of Minerals

Volumn 23, Issue 3, 1996, Pages 173-185

  Petit, P E ^a   Guyot, F ^a,b   Fiquet, G ^c   Itie J P ^d  

^a CNRS   (France)

^b INSTITUT DE PHYSIQUE DU GLOBE DE PARIS   (France)

^c UNIVERSITÉ DE LYON   (France)

^d SORBONNE UNIVERSITÉ   (France)

Author keywords

[No Author keywords available]

Indexed keywords

GERMANATE OLIVINE; HIGH PRESSURE; PHASE TRANSITION; X-RAY ABSORPTION SPECTROSCOPY; XRD;

EID: 0029752414     PISSN: 03421791     EISSN: None     Source Type: Journal    
DOI: 10.1007/BF00220728     Document Type: Article

References (60)

1. 3. Phys Chem Minerals 18:91-105
2. 3 wollastonite. Phys Chem Minerals 18: 506-513
3. 4 olivines: a high-pressure X-ray diffraction study up to 70 GPa. Phys Chem Minerals 22: 99-107
4. 3+ in Garfield notronite: a spectroscopic study. Phys Chem Minerals 12: 55-64
5. 4 with special reference to the olivine-spinem transition. Am J Sci 258: 225-246
6. Dartyge E, Depautex C, Dubuisson JM, Fontaine A, Jucha A, Leboucher P, Tourillon G (1986) X-ray absorption in dispersive mode: a new spectrometer and a data acquisition system for fast kinetics. Nucl Instrum Methods A 246: 452-460
7. 4) crystal and glass. Am Mineral 78: 1143-1148
8. 4. Z Kristallogr 131: 322-341
9. 4 solivines. Phys Chem Minerals 18: 469-479
10. 3. Am Mineral 79: 15-23
11. Furnish MD, Basset WA (1983) Investigation of the mechanism of olivine-spinel transition in fayalite by synchrotron radiation. J Geophys Res 88: 333-342
12. Graham EK, Barsch GR (1969) Elastic constant of single crystal forsterite as a function of temperature and pressure. J Geophys Res 74: 5949-5960
13. Guyot F, Reynard B (1992) Pressure-induced structural modifications and amorphization in olivine compound. In: Bottinga Y, Dingwell DB, Richet P (guest-eds) Silicate Melts, Chem Geol 96: 411-420
14. 4. Geophys Res Lett 18: 89-92
15. Hazen RM (1976) Effects of the temperature and pressure on the crystal structure of forsterite. Am Mineral 61: 1280-1293
16. 4: Insights on the origin of olivine elastic anisotropy. Phys Chem Minerals 14: 13-20
17. Hazen RM, Finger LW (1980) Crystal structure of forsterite at 40 kbar. Carnegie Inst Washington Yearbook 79: 364-367
18. Hemley RJ, Jephcoat AP, Mao HK, Ming LC, Manghnani MH (1988) Pressure-induced amorphization of crystalline silica. Nature 334: 52-54
19. 4) up to 20 kilobars and 1300 degrees C. Phys Earth Planet Inter 14:P3-P5
20. Hofmeister AM, Xu J, Mao HK, Bell PM, Hoering TC (1989) Thermodynamics of Fe-Mg olivines at mantle pressure. Mid-and far-infrared spectroscopy at high pressure Am Mineral 74: 281-306
21. 2 using extended x-ray-absorption fine structure. Phys Rev B 37: 6513-6516
22. Hyde BG, White TJ, O'Keefe M, Johnson AWS (1982) Structures related to those of spinel and the β-phase, and a possible mechanism for the transformation olivine-spinel. Z Kristallogr 160: 53-62
23. Isaak DG, Anderson OL, Goto T, Suzuki I (1989) Elasticity of single-crystal forsterite measured to 1700 K. J Geophys Res 94: 5895-5906
24. Itié JP (1992) X-ray absorption spectroscopy under high pressure. Phase transition 39: 81-98
25. 2. Phys Rev Lett 63: 398-401
26. 3 stoichiometry. Phys Chem Minerals 4: 265-273
27. Jeanloz R (1980) Shock effect in olivine and implication for the Hugoniot data. J Geophys Res 85: 3163-3176
28. Jeanloz R, Ahrens TJ, Lally JS, Nord JL Jr, Christie JM, Heuer AM (1977) Shock-produced olivine glass: first observation. Science 197: 457-459
29. 2. J Appl Phys 49: 5473-5478
30. Jost KH, Ziemer B, Seydel R (1977) Redetermination of the structure of β-dicalcium silicate. Acta Cryst B 33: 1696-1700
31. 4 under high pressure up to 149 kb. Z Kristallogr 171: 291-302
32. Kumazawa M, Anderson OL (1969) Elastic moduli, pressure derivatives and temperature derivatives of single crystal olivine and single crystal forsterite. J Geophys Res 75: 5641-5972
33. Le Toulec R, Pinceaux JP, Loubeyre P (1988) The membrane diamond anvil cell: a new device for generating continuous pressure and temperature variations. High Pressure Research 1: 77-90
34. Liebermann RC (1975) Elasticitiy of olivine (α), beta (β) and spinel (γ) polymorphs of germanates and silicates. Geophys J R Astr Soc 42: 899-929
35. Liu LG (1977) The post-spinel phase of twelve silicates and germanates. In: Manghnani MH, Akimoto S (eds) High-pressure research: Application in geophysics, pp 245-253, Academic Press, New York
36. 4-type structure. Phys Earth Planet Inter 17: 29-33
37. 4 in shocked meteorites: planar defects and polymorphic transitions. Phys Earth Planet Inter 33: 31-44
38. 2 polymorphs. Phys Chem Minerals 18: 7-18
39. Meng Y, Weidner DJ, Fei Y (1993) Deviatoric stress in aquasi-hydrostatic diamond anvil cell: Effect on the volume-based pressure calibration. Geophys Res Lett 20: 1147-1150
40. Nishikawa M, Akimoto S (1971) Bridgman anvil with an internal heating system for phase transformation studies. High TempHigh Press 3: 161-176
41. Polian A, Itié JP, Dartyge E, Fontaine A, Tourillon G (1989) X-ray absorption spectroscopy on solid krypton up to 20 GPa. Phys Rev B 39: 3369-3373
42. Rehr JJ, Albers RC, Zabinsky SI (1992) High-order multiple scattering calculations of X-ray Absorption Fine Structure. Phys Rev Lett 69: 3397-3400
43. Reichlin R (1978) The crystal chemistry of orthogermanates. MSc thesis, State University of New York at Stony Brook, 78 pp
44. 4-olivine: a Raman spectroscopic study. Phys Chem Minerals 20: 556-562
45. 4 liquid. Geophys Res Letters 17: 2093-2096
46. Ringwood AE (1975) Composition and Petrology of the Earth's mantle, 618 pp. McGraw-Hill, New York
47. 4 type. Earth Planet Sci Lett 5: 67-70
48. 4 olivine-spinel phase transition. Phys Chem Minerals 14: 473-481
49. 4. Am Mineral 72: 748-755
50. 4 under pressure. Proc 8th AIRAPT Conf, Uppsala, pp 744-750
51. Soga N (1971) Sound velocity of some germanates compounds and its relation to the law of corresponding states J Geophys Res 76: 3983-3989
52. Sotin C, Madon M (1988) Generalised non-linear inversion of kinetics data: application to the calcite↔aragonite translation. Phys Earth Planet Inter 52: 159-171
53. Stolper EM, Ahrens TJ (1987) On the nature of pressure-induced coordination change in silicate mets and glasses. Geophys Res Lett 14: 1231-1233
54. Teo BK (1986) EXAFS: Basic principles and data analysis. Springer, Berlin Heidelberg New York
55. Tolentino H, Dartyge E, Fontaine A, Tourillon B (1988) X-ray absorption spectroscopy in the dispersive mode with synchrotron radiation: Optical considerations. J Appl Crystallogr 21: 15-21
56. Webb S, Jackson I (1990) Polyhedral rationalization of variation among the single-crystal elastic moduli for the upper-mantle silicate garnet, olivine and orthopyroxene. Am Mineral 75: 731-738
57. 4 and evaluation of elastic analogues. Phys Earth Plane Inter 33. 275-283
58. 4. In: Manghnani MH, Syono Y (eds) High Pressure in Mineral Physics, Geophys Monograph 39, pp 177-186, Terra Scientific Publishing Company Tokyo and AGU Washington
59. Williams Q, Jeanloz R (1989) Static amorphization of anorthite and comparison with diaplectic glass. Nature 338: 413-415
60. 4-fayalite at ultra-high pressures: amorphization and gap closure. J Geophys Res 95: 21 549-21 563