Email this article Modeling method for obtaining kinetic parameters of metamorphic reactions in texture-homogeneous rocks
- Authors: Likhanov I.I.1
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Affiliations:
- V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences
- Issue: Vol 488, No 4 (2019)
- Pages: 420-424
- Section: Geochemistry
- URL: https://journals.eco-vector.com/0869-5652/article/view/17686
- DOI: https://doi.org/10.31857/S0869-56524884420-424
- ID: 17686
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Abstract
A new approach for deriving kinetic parameters of diffusion-controlled metamorphic reactions is described. It is based on comparison of models of temperature field evolution near a cylindrical intrusion and observable chemical changes in minerals at the contact aureole of the Kharlovo massif. The calculations yielded estimates of the effective rates of metamorphic reactions (~10-12 s-1) and the effective diffusion coefficient (5.29 ·10-16 cm2s-1 at T = 475 °С). These values are consistent with experimentally and theoretically derived estimates of solid-state diffusion, including grain-boundary diffusion in mineral aggregates and segregations for the respective PT-parameters.
About the authors
I. I. Likhanov
V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences
Author for correspondence.
Email: likh@igm.nsc.ru
Russian Federation, 3, Koptug prospect, Novosibirsk, 630090
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