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Magnesium K-edge EXAFS study of bond-length behavior in synthetic pyrope-grossular garnet solid solutions

Published/Copyright: April 1, 2015

Abstract

Direct structural characterization of the changes in the local environment of Mg occurring in the garnet structure as a function of the Ca content are determined by Mg K-edge X-ray absorption fine structure on synthetic samples along the pyrope-grossular join. With increasing Ca content, the short Mg-O2 distance of the dodecahedron slightly decreases, while the long Mg-O4 distance tends to increase, so that the dodecahedron is more distorted in grossular-rich garnets than in end-member pyrope. This quantitative direct description of the changes in the local environment of Mg in the pyrope-grossular solid solution confirms and better defines previous experimental and recent computational results.

Received: 2007-10-22
Accepted: 2007-10-30
Published Online: 2015-4-1
Published in Print: 2008-2-1

© 2015 by Walter de Gruyter Berlin/Boston

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Articles in the same Issue

  1. Why is amazonitic K-feldspar an earmark of NYF-type granitic pegmatites? Clues from hybrid pegmatites in Madagascar
  2. Metamorphosed Ordovician Fe- and Mn-rich rocks in south-central Maine: From peri-Gondwanan deposition through Acadian metamorphism
  3. Boralsilite, Al16B6Si2O37, and “boron-mullite:” Compositional variations and associated phases in experiment and nature
  4. Prograde muscovite-rich pseudomorphs as indicators of conditions during metamorphism: An example from NW Maine
  5. Wagnerite in a cordierite-gedrite gneiss: Witness of long-term fluid-rock interaction in the continental crust (Ile d’Yeu, Armorican Massif, France)
  6. Mineral chemistry of Ti-rich biotite from pegmatite and metapelitic granulites of the Kerala Khondalite Belt (southeast India): Petrology and further insight into titanium substitutions
  7. Multiple titanium substitutions in biotites from high-grade metapelitic xenoliths (Euganean Hills, Italy): Complete crystal chemistry and appraisal of petrologic control
  8. Proto-polymorphs of jimthompsonite and chesterite in contact-metamorphosed serpentinites from Japan
  9. Silicate garnet: A micro to macroscopic (re)view
  10. Monazite occurrence, chemistry, and chronology in the granitoid rocks of the Lachlan Fold Belt, Australia: An electron microprobe study
  11. Single-crystal 40Ar/39Ar age variation in muscovite of the Gassetts Schist and associated gneiss, Vermont Appalachians
  12. Single-crystal X-ray studies of trioctahedral micas coexisting with dioctahedral micas in metamorphic sequences from western Maine
  13. Tourmaline chemistry and the IIIB site
  14. The octahedral sheet of metamorphic 2M1-phengites: A combined EMPA and AXANES study
  15. Crystal chemistry of phlogopite from Vulture-S. Michele Subsynthem volcanic rocks (Mt. Vulture, Italy) and volcanological implications
  16. Beneath the Stillwater Complex: Petrology and geochemistry of quartz-plagioclasecordierite (or garnet)-orthopyroxene-biotite ± spinel hornfels, Mountain View area, Montana
  17. Correlation between crystallization pressure and structural parameters of phengites
  18. The modular structure of dovyrenite, Ca6Zr[Si2O7]2(OH)4: Alternate stacking of tobermorite and rosenbuschite-like units
  19. Environmental parameters affect the physical properties of fast-growing magnetosomes
  20. In situ Raman spectroscopy measurements of MgAl2O4 spinel up to 1400 °C
  21. Vibrational properties of δ-AlOOH under pressure
  22. Mössbauer spectroscopic study of synthetic leucophosphite, KFe2(PO4)2(OH)·2H2O
  23. Rhönite in Luna 24 pyroxenes: First find from the Moon, and implications for volatiles in planetary magmas
  24. New high-pressure B2 phase of FeS above 180 GPa
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