Abstract
Crystal size distributions (CSDs) provide information about the nucleation and growth conditions of crystals. In the present study, we investigated CSDs of garnets in metapelites in the Bushveld contact aureole to examine the mechanisms of garnet nucleation and growth and to deduce controlling factors of CSDs. The CSD shapes were evaluated in terms of the Law of Proportionate Effects crystal growth and of the thermally accelerated, diffusion-controlled nucleation and growth. We adopted both the nonparametric and parametric stereological methods to estimate three-dimensional crystal size distributions from two-dimensional measurements of crystal diameters. The studied garnets showed various CSD shapes: asymptotic, lognormal, and near-symmetric distributions. These varieties of CSDs are generally controlled by heating rate, metamorphic temperature, and duration of thermal effects due to the intrusion of the igneous body, the Rustenburg Layered Suites. The chemical composition of the host sedimentary rocks is an additional important factor in controlling CSD shapes: it affects garnet growth as a supply source of nutrients for the mineral. At the contact between the Rustenburg igneous rocks and the aureole, where a rapid increase of temperature and a migmatitic extraction of siliceous melts occurred, the CSD is asymptotic showing constant- or accelerating-nucleation rates. In contrast, at some distance from the igneous contact where a relatively slower rise of temperature occurred and lognormal to near symmetric CSDs were mainly generated, suggesting decaying-rate nucleation dominated. However, even in such thermal conditions, differences in chemical compositions of host rocks affected growth mechanisms of garnet porphyroblasts, which resulted in relatively symmetric and pseudo-lognormal CSDs of garnets in biotite- and quartz-rich layers, respectively, in a pelitic sample
© 2015 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
- Crystal-size and shape distributions of magnetite from uncultured magnetotactic bacteria as a potential biomarker
- Tourmaline-bearing rocks in the Singhbhum shear zone, eastern India: Evidence of boron infiltration during regional metamorphism
- High-resolution transmission electron microscopy (HRTEM) study of the 4a and 6a superstructure of bornite Cu5FeS4
- Possible Fe/Cu ordering schemes in the 2a superstructure of bornite (Cu5FeS4)
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- Dehydration processes in the meta-autunite group minerals meta-autunite, metasaléeite, and metatorbernite
- Investigation of the martensitic-like transformation from Mg2GeO4 olivine to its spinel structure polymorph
- A high-temperature diffraction study of the solid solution CaTiOSiO4-CaTiOGeO4
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- Synthesis and crystal-chemistry of alkali amphiboles in the system Na2O-MgO-FeO-Fe2O3- SiO2-H2O as a function of fO2
- Compositional zoning in sphalerite crystals
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