• journal_title：American Mineralogist
• Contributor：Roberta Oberti ; Simona Quartieri ; Maria Chiara Dalconi ; Federico Boscherini ; Gianluca Iezzi ; Massimo Boiocchi ; Sigrid Griet Eeckhout
• Publisher：Mineralogical Society of America
• Date：2006-
• Format：text/html
• Language：en
• Identifier：10.2138/am.2006.2037
• journal_abbrev：American Mineralogist
• issn：0003-004X
• volume：91
• issue：8-9
• firstpage：1230
• section：Articles

We applied different independent techniques (electron microprobe analysis, structure refinement, and X-ray absorption spectroscopy) to unravel the possible mechanisms of Sc incorporation in the pyrope-grossular join. Samples were synthesized at elevated pressure and temperature by adding 5 wt% of Sc₂O₃ to selected nominal compositions (pyrope, pyrope₆₀grossular₄₀, pyrope₂₀grossular₈₀, and grossular). In this way, the site of incorporation was not pre-determined, and only depends on the availability of a mechanism for local charge-balance. The EXAFS spectra of the two end-members could be analyzed by a multi-shell fit procedure, whereas the chemical heterogeneity of the Sc-doped solid-solution terms prevented this approach. However, the available information allows detection of different mechanisms of incorporation, which are active as a function of the bulk composition. In pyrope, Sc mainly enters the dodecahedral X site, and the local charge balance is achieved by incorporation of Mg at the adjacent tetrahedral Z site. Local charge-balance requirements suggest that a Z site occupied by Mg bridges two X sites occupied by Sc. When the entrance of Ca provides relaxation of the averaged structure, Sc may enter all the three available cation sites via the coupled heterovalent exchange ^XSc₁^ZSc₁^XMg₋₁^ZSi₋₁ and the homovalent exchange ^YSc₁^YAl₋₁. In the samples of this work, there is an apparent limit in the Sc incorporation at the Y site, which is in contrast to the favored mechanism of incorporation in Sc-doped andradites. This limit can be explained in terms of relative dimensions of the structural sites when Al is the dominant Y cation. These results must be taken into account when evaluating trace-element behavior in garnets for geochemical purposes. In particular, they explain why D_Sc can be treated together with D_REE in models based on the elastic strain theory in garnets close to the pyrope composition, but deviate from the parabolic fit in grossular-rich garnets.