TRACE ELEMENT ZONING IN TITANITE FROM SYROS, GREECE: IMPLICATIONS FOR COUPLED SUBSTITUTION MECHANISMS
Trace element concentrations in titanite were determined by LA-ICP-QQQ-MS using a NWR193UC excimer laser ablation system coupled with an Agilent 8900 mass spectrometer at the University of Maine MAGIC Laboratory. Concentrations in titanite were determined relative to the NIST610 glass reference material. NIST612 glass and BLR-1 titanite were analyzed as quality control materials. Major and trace element concentrations in titanite show two distinct zones: (1) high-Al cores enriched in Rb, Y, and HREE, and (2) low-Al rims enriched in Na, Sr, Nb, Ta, and LREE. In a closed system, decreasing Rb, Y, and HREE may reflect fractionation of trace elements during titanite growth; however, in an open system they may also be a function of changing trace element partitioning conditions (i.e., a trace element response to metasomatic replacement) or an evolving fluid composition. Increased Nb and Ta in titanite rims is likely related to rutile breakdown during rind formation. Additionally, positive correlation of Nb with Na and negative correlation of Nb with Al + Fe suggests the coupled substitution of Nb5+ plus Na+ for Ti4+ plus Ca2+. This contrasts with the proposed substitution for 5+ cations (e.g., Nb, Ta) in titanite which is balanced by (Al, Fe)3+ for two Ti4+ cations.