Big Chemical Encyclopedia

Chemical substances, components, reactions, process design ...

Articles Figures Tables About

High albite

Fig. 2.39. Na /K+ atomic ratios of well discharges plotted at measured downhole temperatures. Curve A is the least squares fit of the data points above 80°C. Curve B is another emperical curve (from Truesdell, 1976). Curves C and D show the approximate locations of the low albite-microcline and high albite-sanidine lines derived from thermodynamic data (from Fournier, 1981). Small solid subaerial geothermal water Solid square Okinawa Jade Open square South Mariana Through Solid circle East Pacific Rise 11°N Open circle Mid Atlantic Ridge, TAG. Fig. 2.39. Na /K+ atomic ratios of well discharges plotted at measured downhole temperatures. Curve A is the least squares fit of the data points above 80°C. Curve B is another emperical curve (from Truesdell, 1976). Curves C and D show the approximate locations of the low albite-microcline and high albite-sanidine lines derived from thermodynamic data (from Fournier, 1981). Small solid subaerial geothermal water Solid square Okinawa Jade Open square South Mariana Through Solid circle East Pacific Rise 11°N Open circle Mid Atlantic Ridge, TAG.
Name High Albite Low Albite Anorthite Celsian... [Pg.352]

Extrapolation at the 2) and 2) of reference of the change in enthalpy between low albite and high albite, determined as a continuous function of ordering parameter Q. [Pg.355]

Figure 5,59 Effects of structural and coherence state on extent of unmixing in the NaAl-Si308-KAlSi30g binary join. (A) Maximum microcline-low albite, based on data from Bachinski and Muller (1971) and Yund (1974). (B) Sanidine-high albite, based on data from Thompson and Waldbaum (1969) and Sipling and Yund (1976). Figure 5,59 Effects of structural and coherence state on extent of unmixing in the NaAl-Si308-KAlSi30g binary join. (A) Maximum microcline-low albite, based on data from Bachinski and Muller (1971) and Yund (1974). (B) Sanidine-high albite, based on data from Thompson and Waldbaum (1969) and Sipling and Yund (1976).
Kroll H., Bambauer H. U., and Schirmer U. (1980). The high albite-monalbite and analbite-monalbite transitions. Amer. Mineral, 65 1192-1211. [Pg.840]

Sipling R J. and Yund R. A. (1976). Experimental determination of the coherent solvus for sanidine-high albite. Amer. Mineral, 61 897-906. [Pg.854]

Winter J. K., Okamura F. P. and Ghose S. (1979). A high temperature structural study of high albite, monalbite, and the analbite-monalbite phase transition. Amer. Mineral, 64 409-423. [Pg.860]

Fig. 2. Activity-composition relationships for sanidine-high albite solid solutions at TOQOC. Fig. 2. Activity-composition relationships for sanidine-high albite solid solutions at TOQOC.
Waldbaum and Thompson (1969). The mixing properties for sanidine -high albite solutions derived by Thompson and Waldbaum (1969a) are used to construct feldspar phase diagrams. The equations of state for alkali feldspar are used to predict equilibria involving reactions among feldspar and other phases (including feldspar liquids) at various temperatures and pressures. [Pg.86]

Zn-Co olivine, and KAlSi3O0 (sanidine) - NaAlSi308 (high albite). (cf. Carlson and Colbiurn, 19 2, and Green, 1970a, b). [Pg.89]

See other pages where High albite is mentioned: [Pg.444]    [Pg.350]    [Pg.354]    [Pg.360]    [Pg.360]    [Pg.362]    [Pg.363]    [Pg.364]    [Pg.129]    [Pg.236]    [Pg.113]    [Pg.784]    [Pg.776]    [Pg.326]    [Pg.132]    [Pg.26]    [Pg.758]    [Pg.872]    [Pg.822]    [Pg.88]    [Pg.90]    [Pg.220]    [Pg.870]    [Pg.775]    [Pg.438]    [Pg.438]    [Pg.438]    [Pg.440]    [Pg.440]    [Pg.440]    [Pg.440]    [Pg.440]    [Pg.440]    [Pg.440]    [Pg.443]   


SEARCH



Albit

Albite

© 2024 chempedia.info