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Species diffusion in clinopyroxene solid solution in the diopside-anorthite system.


ABSTRACT: The coupled multicomponent diffusion of the species Ca2Si2O6, CaAl2SiO6 and Mg2Si2O6 was determined in diopside crystals in the diopside/anorthite (Di/An) system at temperatures (T) of 1110-1260 °C and oxygen fugacities (fO 2 ) between 1.0 log unit below and above the fayalite-magnetite-quartz equilibrium (FMQ?±?1). Diffusion couples were prepared by the seed overgrowth technique. Element concentration profiles were measured perpendicular to the rim/core interface by step-scanning profiling with a field emission gun scanning electron microscope (FEG-SEM). The multicomponent diffusion matrix was solved by fitting its eigenvalues (?) and eigenvectors (v) to the measured concentration profiles. The full diffusion matrix D can be recovered by using the formula D = P ? P - 1 resulting in the following equation: D Di/An = 1.00 - 0.67 - 0.38 1.00 ? 1 T 0 0 ? 2 T 1.00 - 0.67 - 0.38 1.00 - 1 . The eigenvalues (?1 and ?2) represent upper limit values and are described by the following Arrhenius-type equations: ? 1 Di/An = 10 - 15.98 ± 1.17 × exp - 114.4 ± 32.8 kJ/mol RT , ? 2 Di/An = 10 - 16.23 ± 1.17 × exp - 114.4 ± 32.8 kJ/mol RT , where ?1 and ?2 are the first and second eigenvalue of the diffusion matrix in m2 s-1 , R is the gas constant and T is the temperature in K. The dominant eigenvalue (?1) is one quarter order of magnitude larger than the second eigenvalue (?2). The eigenvectors are constant for all experiments inferring that the entire D matrix can be described with the eigenvalues as the only T-dependent parameter. Additionally, the derived diffusion data and modeling approach were applied to constrain the duration of magmatic processes recorded in zoned clinopyroxene (cpx) phenocrysts from a basaltic, post-plutonic dyke of the Tertiary Adamello batholiths (N-Italy). The results reveal residence times of the overgrown cpx prior to final emplacement in the range of 0.25-1.7 years (lower limit values) testifying that the data and method can be applied to model cpx diffusion profiles in complex natural cpx.

SUBMITTER: Lierenfeld MB 

PROVIDER: S-EPMC6515693 | biostudies-literature | 2019

REPOSITORIES: biostudies-literature

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Species diffusion in clinopyroxene solid solution in the diopside-anorthite system.

Lierenfeld Matthias Bernhard MB   Zhong Xin X   Reusser Eric E   Kunze Karsten K   Putlitz Benita B   Ulmer Peter P  

Contributions to mineralogy and petrology. Beitrage zur Mineralogie und Petrologie 20190513 5


The coupled multicomponent diffusion of the species Ca<sub>2</sub>Si<sub>2</sub>O<sub>6</sub>, CaAl<sub>2</sub>SiO<sub>6</sub> and Mg<sub>2</sub>Si<sub>2</sub>O<sub>6</sub> was determined in diopside crystals in the diopside/anorthite (Di/An) system at temperatures (<i>T</i>) of 1110-1260 °C and oxygen fugacities (<i>fO</i> <sub><i>2</i></sub> ) between 1.0 log unit below and above the fayalite-magnetite-quartz equilibrium (FMQ ± 1). Diffusion couples were prepared by the seed overgrowth techniq  ...[more]

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