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Analyzing Crystal Fractionation. Phoenix Polar Lander. Le Castor. Curiosity Gale Crater.

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Analyzing

Crystal Fractionation

Phoenix

Polar Lander

Le Castor

Curiosity

Gale Crater


Four component systems are insufficient to accurately portray the phase relations of primary magmas as they evolve due to processes such as crystal fractionation. For example, we cannot determine when an oxide mineral will crystallize in the olivine liquidus projection to the left.

One solution to this problem is the use of binary variation diagrams to study liquid lines of descent in volcanic suites.


Mg variation diagrams (Bowen Diagrams): portray the phase relations of primary magmas as they evolve due to processes such as crystal fractionation. For example, we cannot determine when an oxide mineral will crystallize in the olivine liquidus projection to the left.

Mg is an analogue for temperature, so that plotting other elements against Mg, gives one an idea of how these elements change as temperature drops during crystal fractionation. This type of diagram is most commonly used in suites with relatively primitive Mg-rich lavas, and is less useful for volcanic suites dominated by relatively felsic lavas.


Vanuatu Arc portray the phase relations of primary magmas as they evolve due to processes such as crystal fractionation. For example, we cannot determine when an oxide mineral will crystallize in the olivine liquidus projection to the left.

Epi


Appearance of Cpx portray the phase relations of primary magmas as they evolve due to processes such as crystal fractionation. For example, we cannot determine when an oxide mineral will crystallize in the olivine liquidus projection to the left.


Appearance of Ulvo-spinel (Fe portray the phase relations of primary magmas as they evolve due to processes such as crystal fractionation. For example, we cannot determine when an oxide mineral will crystallize in the olivine liquidus projection to the left.2TiO4)


Appearance of Apatite as a Liquidus Phase portray the phase relations of primary magmas as they evolve due to processes such as crystal fractionation. For example, we cannot determine when an oxide mineral will crystallize in the olivine liquidus projection to the left.

In Marquesa Archipelago


Analyzing Crystal Cumulates Using Pearce element Ratios portray the phase relations of primary magmas as they evolve due to processes such as crystal fractionation. For example, we cannot determine when an oxide mineral will crystallize in the olivine liquidus projection to the left.

1:1

2:1

1:2

amphibolites


Olivine + Cpx portray the phase relations of primary magmas as they evolve due to processes such as crystal fractionation. For example, we cannot determine when an oxide mineral will crystallize in the olivine liquidus projection to the left.

XCpx versus Yolivine


Estimating degree of crystallization using highly incompatible elements:

Incompatible elements are those that preferentially partition into a liquid phase coexisting with solid phases. They tend to be elements whose high charge (HFSE, high field strength elements such as: Zr, Nb, Hf) or large ionic radii (LIL, large ion lithophile elements such as: Rb, Ba, La), prevent them from substituting for the common major elements. For any trace element i:

Ki = Cisolid / Ciliq

at equilibrium:

Cio = Fliq× Ciliq + (1-Fliq) × Cisol

Cio = Fliq× Ciliq + (1-Filiq) × Ki × Ciliq

Cio = Fliq× Ciliq if Ki = 0

Fliq = Cio / Ciliq

or

Xxyl = 1- (Cio / Ciliq)


For K incompatible elements:i≠ 0.0

In the case of one crystallizing mineral:

Ciliq = Cio / ((F + Ki×(1-F)) for equilibrium crystallization

Ciliq = Cio × F(Ki -1) for fractional crystallization

In the case of 2 or more crystallizing minerals:

Ciliq = Cio / ((F + Di×(1-F)) for equilibrium crystallization

Ciliq = Cio × F(Di -1) for fractional crystallization

Di = Xα× Kiα + Xβ × Kiβ + Xγ × Kiδ+ …….. where ∑n Xn = 1


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