Testing the Crystalline Integrity of Baddeleyite: A Systematic EBSD and Confocal Laser-Raman Spectroscopy Study
Abstract
The accessory mineral baddeleyite (monoclinic ZrO2) has great potential as a high-precision U-Pb geochronometer in silica-undersaturated rocks. However, due to a lack of understanding of alpha-recoil damage to the crystal structure and the influences on chemical diffusion properties and closed-system behavior, limitations still exist. Studies have shown phase transformations in baddeleyite (monoclinic to tetragonal) resulting from radiation damage due to ion bombardment [e.g., 1], but the effects of self-irradiation on the baddeleyite crystal structure over geologic timescales remain poorly understood. A recent study reported confocal laser-Raman spectra suggesting the presence of a tetragonal phase in a Phalaborwa baddeleyite [2], which has crucial implications for Pb mobility and high-precision U-Pb results. To better understand the physical effects of self-irradiation in baddeleyite over geologic timescales, samples of various ages (ca. 2060-32 Ma) and calculated alpha-doses (0.001-0.901 x 1016 α/mg) were imaged by cathodoluminescence (CL) and subsequently analyzed via electron backscatter diffraction (EBSD) and confocal laser-Raman spectroscopy. Synthetic baddeleyite grown in a one-atmosphere furnace was also analyzed to allow a comparison of EBSD and Raman results of the pure monoclinic phase and the natural unknown samples. Whole grain EBSD maps (n=75) of baddeleyite from the Phalabowra and Kovdor carbonatites, the Ammänpelto sill, and the Duluth, Ogden and Yinmawanshan gabbros show complex twinning that is loosely correlated to CL zoning and identification of the monoclinic phase only, suggesting no evidence for phase transformations within grains of contrasting age and amounts of alpha-doses. Preliminary Raman results show evidence of systematic shifts in the vibrational modes of Phalabowra baddeleyite with respect to the younger crystals, which may be the result of radiation-induced damage accumulation rather than phase transformation. These results aim to better characterize the poorly known effects of radiation damage in natural baddeleyite and assist in improving methods for high-precision U-Pb dating of mafic systems on Earth and other planetary bodies. [1] Valdez et al. (2008), J. Nucl. Mater. 381, pp. 259-266. [2[ Schaltegger and Davies (2017), RIMG 83, pp.297-328.
- Publication:
-
AGU Fall Meeting Abstracts
- Pub Date:
- December 2017
- Bibcode:
- 2017AGUFM.V13B0379D
- Keywords:
-
- 1140 Thermochronology;
- GEOCHRONOLOGY;
- 1160 Planetary and lunar geochronology;
- GEOCHRONOLOGY;
- 3640 Igneous petrology;
- MINERALOGY AND PETROLOGY;
- 3660 Metamorphic petrology;
- MINERALOGY AND PETROLOGY