Estimation of based on Fe-Mg exchange in olivine-orthopyroxene in magnetite buffered assemblages
This is based on the following equilibrium (see classic paper of Frost 1982, JPet)
(1)
Oxygen fugacity can be expressed as follows
[Eq. 1]
In order to derive this expression, let's start as
where
and
the activity of is
but we want units instead so,
[Eq. 1]
Formal derivation
The above treatment is obscure in the definition of because it is calculated at the P,T conditions for all endmembers except for that is computed at 1 bar. The derivation is as follows
(1)
for this reaction in solid solution we have
Which is strictly
then
but noting that
that simplifies to
then
we normally report this value as , that by definition is