Olivier Bachmann and Michael A. Dungan
Temperatureinduced Alzoning in hornblendes of the Fish Canyon magma, Colorado 1062
Item #AM02014
Bachmann_p1062_02_Append1a.pdf (140 K)
Bachmann_p1062_02_Append1b.pdf (148 K)
Bachmann_p1062_02_Append1c.pdf (128 K)
Bachmann_p1062_02_Append1d.pdf (128 K)
Bachmann_p1062_02_Append1e.pdf (108 K)
Bachmann_p1062_02_Append1f.pdf (148 K)
Bachmann_p1062_02_Append1g.pdf (124 K)
APPENDIX FIGURE 1. All microprobe profiles in hornblendes from all the different stratigraphic units of the Fish Canyon
magmatic system (see Fig. 2 for a subset of six profiles).
Bachmann_p1062_02_Append2a.pdf (32 K)
Bachmann_p1062_02_Append2b.pdf (32 K)
APPENDIX FIGURE 2. Frequency distribution diagram of pressure calculated for the low and highAl populations using the
equation from AS1995. For the lowAl population, pressures were calculated for both 700 and 760 °C, considered to be the two
endmember temperatures of the range over which the Fish Canyon hornblende crystallized. Also reported is the estimate of
mineral equilibration pressure of Johnson and Rutherford (1989a; 2.4 ± 0.5 kbar). 2: T Al vs. A (Na + K) plots for each traverse
across hornblende reported in Appendix 1, designed to estimate the contribution of the edenite substitution in the total T Al
variation. The slopes of the regression lines consistently around 0.5 illustrate that the edenite exchange accounts for half of the
total T Al variation for all analyzed phenocrysts.
Bachmann_p1062_02_Append3.pdf (48 K)
APPENDIX FIGURE 3. Frequency distribution diagrams of temperature calculated for the lowAl and highAl populations
designed to show the influence of the input parameters P and XAb in the HB1994TB (left), HB1994TA (right) and BH1990
(bottom) calibrations of the Alinhornblende thermometer.
Bachmann_p1062_02_Append4.pdf (16 K)
APPENDIX FIGURE 4. Frequency distribution diagrams of pressure calculated for the low and highAl populations at different
temperature using the equation of AS1995. These diagrams demonstrate how sensitive the algorithm is to small changes in
temperature.
Bachmann_p1062_02_Append5.xls (1 MB)
APPENDIX FIGURE 5. Major element analyses and structural formulae (13eCNK) of the 2146 electron microprobe analyses
of the data set.
Paolo Ballirano, Athos Callegari, Franca Caucia, Adriana Maras, Fiorenzo Mazzi, and Luciano Ungaretti
The crystal structure of vicanite(Ce), a borosilicate showing an unusual (Si_{3}B_{3}O_{18})^{15} polyanion 1139
Item #AM02012
Ballirano_p1139_02_Table56.pdf (48 K)
Table 5. Anisotropic displacement coefficients (x 10^{4}) in vicanite(Ce).
Table 6. Observed (Fo) and calculated (Fc) structure factors in vicanite(Ce).
Paola Comodi, Michela Montagnoli, Pier Francesco Zanazzi, and Tiziana Boffa Ballaran
Isothermal compression of staurolite: A singlecrystal study 1164
Item #AM02013
Comodi_p1164_02_Table4.doc Word document (188 K)
Table 4a. Observed and calculated structure factors for staurolite (Sp. Gr. C2/m) in air.
Table 4b. Observed and calculated structure factors for staurolite (Sp. Gr. Ccmm).
Table 4c. Observed and calculated structure factors for staurolite (Sp. Gr. Ccmm) at 2.48 GPa.
Table 4d. Observed and calculated structure factors for staurolite (Sp. Gr. Ccmm) at 4.15 GPa.
Table 4e. Observed and calculated structure factors for staurolite (Sp. Gr. Ccmm) at 5.43 GPa.
Table 4f. Observed and calculated structure factors for staurolite (Sp. Gr. Ccmm) at 6.84 GPa.
Table 4g. Observed and calculated structure factors for staurolite (Sp. Gr. Ccmm) at 8.74 GPa.
