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Week 6: Feb
20 and 22
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Compositional variation in minerals (cont'd
...)
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Exsolution - ("unmixing") the process
whereby an initially homogenous solid solution separates into 2 (or more)
distinct crystalline phases. This may occur with a drop in T from higher
T where solid solution is favored to lower T where it is not.
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exsolution requires ions to move and segregate
into the two different crystalline domains
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exsolution textures in minerals may take the
form of lamellae, "blebs", stringers, rods, etc.
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example: at high T alkali feldspar--(Na,K)AlSi3O8--
shows complete solid solution between albite--NaAlSi3O8 and K-feldspar--KAlSi3O8
wherein there are no restrictions on the amount of Na and K in the mineral.
At lower T, however, albite-rich lamellae begin to segregate from K-f rich
host along the {100} plane
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(subsolidus) phase diagram for alkali feldspar
showing variation in composition of exsolving domains (see Fig. 5.23 of
Nesse)
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(subsolidus) phase diagram for plagioclase
(NaAlSi3O8-CaAl2Si2O8) showing the peristerite and Boggild-Huttenlocher
miscibility gaps.
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Zoning - The (usually) concentric variation
of composition in a crystal having solid solution. The core usually has
a composition that was in equilibrium with the liquid (or some other matrix
as in a metamorphic rock) at higher T, and the rim has a lower T composition.
The reverse may also occur.
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example: zoning in plagioclase
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plagioclase phase diagram (see fig. 5.10 of
Nesse)
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Growth of Minerals
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stable, unstable, and metastable states
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Gibbs Free Energy and mineral stability -
the mineral assemblage with the lowest Gibbs free energy is the stable
assemblage
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Gibbs free energy is a function of pressure
and temperature; since P and T affect the Gibbs free energy of each mineral
differently, some minerals will have a lower free energy than others and
will end up being more stable.
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Homogenous vs. heterogenous nucleation
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Role of defects in aiding crystal growth
Mineralogy
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