Abstract
The ubiquity of quartz in continental crust, and the involvement of SiO2 in multiple metamorphic processes such as reactions, fluid flux, and solution-transfer processes, makes quartz an obvious choice for reconstructing prograde metamorphic conditions in various rock types. Recent studies have shown the usefulness of analyzing Ti distribution in quartz to constrain pressure-temperature-(relative) timedeformation (P-T-t-D) in metamorphosed tectonites. New high-precision single-crystal X‑ray diffraction volume constraints on Ti-doped and chemically pure quartz provide further evidence for substitution of Ti4+ for Si4+ in the tetrahedral site in quartz, with resultant lattice strain on the structure.
Recent applications of the Ti-in-quartz thermobarometer to dynamically recrystallized quartz have identified recrystallized subgrains that contain lower Ti concentrations ([Ti]) than their host porphyroclasts. In addition, [Ti] are lower than expected for the temperatures of recrystallization. Atomistic simulations that estimate energetic perturbations resulting from Ti incorporation into the quartz lattice indicate that significant increases in strain energy occur only at very high [Ti]; the strain-energy increase is negligible for [Ti] typical of quartz grown under mid-crustal conditions. This suggests that lattice strain rarely provides an appreciable driving force for Ti loss from quartz; instead, it appears that subgrain boundaries and dislocation arrays migrating through recrystallizing quartz crystals can promote localized re-equilibration, thermodynamically regulated by the composition of the intergranular medium (typically undersaturated in Ti). It therefore appears that analyses from dynamically recrystallized quartz cannot be meaningfully interpreted until methods are developed that can account quantitatively for the reduction of Ti resulting from crystal plastic flow.
© 2014 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
- Highlights and Breakthroughs. Pauling’s rules, in a world of non-spherical atoms
- Highlights and Breakthroughs. Theoretical and applied implications of the structural order of irradiated vermiculite
- Highlights and Breakthroughs. An examination of the Ti-in-quartz thermobarometer in rocks that contain dynamically recrystallized quartz: Re-equilibration of [Ti] during recrystallization
- The Second Conference on the Lunar Highlands Crust and New Directions. Visible-infrared spectral properties of iron-bearing aluminate spinel under lunar-like redox conditions
- The Second Conference on the Lunar Highlands Crust and New Directions. VNIR spectral variability of the igneous stratified Stillwater Complex: A tool to map lunar highlands
- The Second Conference on the Lunar Highlands Crust and New Directions. Spinel-rich lithologies in the lunar highland crust: Linking lunar samples with crystallization experiments and remote sensing
- The Second Conference on the Lunar Highlands Crust and New Directions. Phosphate-halogen metasomatism of lunar granulite 79215: Impact-induced fractionation of volatiles and incompatible elements
- The Second Conference on the Lunar Highlands Crust and New Directions. Reflectance spectroscopy of plagioclase-dominated mineral mixtures: Implications for characterizing lunar anorthosites remotely
- The Second Conference on the Lunar Highlands Crust and New Directions. The distribution of Mg-spinel across the Moon and constraints on crustal origin
- The occurrence and composition of chevkinite-(Ce) and perrierite-(Ce) in tholeiitic intrusive rocks and lunar mare basalt
- Garnet as a major carrier of the Y and REE in the granitic rocks: An example from the layered anorogenic granite in the Brno Batholith, Czech Republic
- Mid-infrared optical constants of clinopyroxene and orthoclase derived from oriented single-crystal reflectance spectra
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- Ab initio investigations of dioctahedral interlayer-deficient mica: Modeling particles of illite found within gas shale
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