Lecture 8 OVERVIEW
Composition space
Two-component systems (linear composition space)
FeO Ð SiO2
Fe2SiO4
Ð Mg2SiO4
Three component systems (planar triangle)
FeO-MgO-SiO2
MgSiO3-FeSiO3-CaSiO3
Chemical
reactions between different mineral phases. EX:
The
minerals that we find together in a given rock are a function of (1) which
mineral or combination of minerals is stable, and (2) the bulk composition of
the rock.
One more
ternary example: CaO-SiO2-Al2O3
Mineral |
Moles
CaO |
Moles
Al2O3 |
Moles
SiO2 |
% CaO |
% Al2O3 |
%SiO2 |
anorthite |
1 |
1 |
2 |
25 |
25 |
50 |
grossular |
3 |
1 |
3 |
43 |
14 |
43 |
wollastonite |
1 |
|
1 |
|
|
|
kyanite |
|
1 |
1 |
|
|
|