Home Crystal-size distributions of garnets in metapelites from the northeastern Bushveld contact aureole, South Africa
Article
Licensed
Unlicensed Requires Authentication

Crystal-size distributions of garnets in metapelites from the northeastern Bushveld contact aureole, South Africa

  • Yasunari Kaneko EMAIL logo , Toshiaki Tsunogae and Takashi Miyano
Published/Copyright: March 28, 2015
Become an author with De Gruyter Brill

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

Received: 2004-4-4
Accepted: 2005-2-13
Published Online: 2015-3-28
Published in Print: 2005-8-1

© 2015 by Walter de Gruyter Berlin/Boston

Articles in the same Issue

  1. Crystal-size and shape distributions of magnetite from uncultured magnetotactic bacteria as a potential biomarker
  2. Tourmaline-bearing rocks in the Singhbhum shear zone, eastern India: Evidence of boron infiltration during regional metamorphism
  3. High-resolution transmission electron microscopy (HRTEM) study of the 4a and 6a superstructure of bornite Cu5FeS4
  4. Possible Fe/Cu ordering schemes in the 2a superstructure of bornite (Cu5FeS4)
  5. TEM-specimen preparation of cell/mineral interfaces by Focused Ion Beam milling
  6. Direct observation of spinodal decomposition in the magnetite-hercynite system by susceptibility measurements and transmission electron microscopy
  7. Thermodynamics of uranyl minerals: Enthalpies of formation of rutherfordine, UO2CO3, andersonite, Na2CaUO2(CO3)3(H2O)5, and grimselite, K3NaUO2(CO3)3H2O
  8. Mixing and ordering behavior in manganocolumbite-ferrocolumbite solid solution: A single-crystal X-ray diffraction study
  9. Structure change of MgSiO3, MgGeO3, and MgTiO3 ilmenites under compression
  10. Dehydration processes in the meta-autunite group minerals meta-autunite, metasaléeite, and metatorbernite
  11. Investigation of the martensitic-like transformation from Mg2GeO4 olivine to its spinel structure polymorph
  12. A high-temperature diffraction study of the solid solution CaTiOSiO4-CaTiOGeO4
  13. The vibrational spectrum of synthetic hydrogrossular (katoite) Ca3Al2(O4H4)3: A low-temperature IR and Raman spectroscopic study
  14. Structural characterization of biogenic Mn oxides produced in seawater by the marine bacillus sp. strain SG-1
  15. Investigation of smectite hydration properties by modeling experimental X-ray diffraction patterns: Part I. Montmorillonite hydration properties
  16. Synthesis and crystal-chemistry of alkali amphiboles in the system Na2O-MgO-FeO-Fe2O3- SiO2-H2O as a function of fO2
  17. Compositional zoning in sphalerite crystals
  18. Structure and the extent of disorder in quaternary (Ca-Mg and Ca-Na) aluminosilicate glasses and melts
  19. Makarochkinite, Ca2Fe42+Fe3+TiSi4BeAlO20, a new beryllosilicate member of the aenigmatite-sapphirine-surinamite group from the Ilʼmen Mountains (southern Urals), Russia
  20. Formation of lava stalactites in the master tube of the 1792-1793 flow field, Mt. Etna (Italy)
  21. Crystal-size distributions of garnets in metapelites from the northeastern Bushveld contact aureole, South Africa
  22. Early diagenetic origin of Al phosphate-sulfate minerals (woodhouseite and crandallite series) in terrestrial sandstones, Nova Scotia, Canada
  23. Scandium silicates from the Baveno and Cuasso al Monte NYF-granites, Southern Alps (Italy): Mineralogy and genetic inferences
  24. Letter. The effect of Fictive temperature on Al coordination in high-pressure (10 GPa) sodium aluminosilicate glasses
  25. Letter. α-PbO2-type nanophase of TiO2 from coesite-bearing eclogite in the Dabie Mountains, China
  26. Letter. Morphological characteristics of ordered kaolinite: Investigation using electron back-scattered diffraction
Downloaded on 14.9.2025 from https://www.degruyterbrill.com/document/doi/10.2138/am.2005.1666/html
Scroll to top button