Thermal annealing kinetics of induced fission tracks in ZAD zircon from the Serra Geral Volcanic Complex, Brazil

IF 1.6 4区 地球科学 Q4 MATERIALS SCIENCE, MULTIDISCIPLINARY
Antonio Said Webbe Sales, Airton Natanael Coelho Dias, Sandro Guedes, Marcela Guinther Medeiros, Vinicius de Queirós Pereira
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Abstract

This study investigates the thermal annealing kinetics of induced fission tracks in ZAD zircon from the Serra Geral Volcanic Complex, Brazil, and compares results with previously studied ZPC zircon. Both samples underwent identical pre-annealing treatment (1100 °C for 1 h) to remove fossil fission tracks before neutron irradiation and heating experiments at temperatures between 500 and 800 °C for durations of 1–100 h. Comprehensive statistical analysis, including Kolmogorov–Smirnov tests and effect size calculations, confirmed that observed differences between samples reflect genuine material properties rather than measurement bias. ZAD exhibited significantly higher annealing rates and lower activation energy (62 ± 14 kcal/mol) compared to ZPC (80 ± 20 kcal/mol), despite both samples undergoing identical laboratory procedures. This differential behavior is attributed to ZAD’s 20% higher accumulated α-recoil damage (3.34 × 1016 vs. 2.67 × 1016 decays/g), which persists as residual damage even after pre-annealing treatment. Calculations of displacements per atom (dpa) further quantified this difference (1.07 × 10−3 for ZAD vs. 8.5 × −4 for ZPC). The study demonstrates how radiation damage accumulated over different timescales (134 Ma for ZAD vs. 80 Ma for ZPC) creates distinct microstructural defect patterns that significantly influence fission track annealing kinetics, with important implications for zircon thermochronology interpretations and geological thermal history reconstruction.

巴西Serra Geral火山杂岩ZAD锆石诱导裂变径迹的热退火动力学
本文研究了巴西Serra Geral火山杂岩中ZAD锆石诱导裂变径迹的热退火动力学,并将结果与之前研究的ZPC锆石进行了比较。两个样品都进行了相同的预退火处理(1100°C 1小时),以去除化石裂变痕迹,然后进行中子辐照和500至800°C加热实验,持续时间为1 - 100小时。综合统计分析,包括Kolmogorov-Smirnov测试和效应大小计算,证实了观察到的样品之间的差异反映了真实的材料特性,而不是测量偏差。与ZPC(80±20 kcal/mol)相比,ZAD表现出更高的退火速率和更低的活化能(62±14 kcal/mol),尽管两种样品经过相同的实验室程序。这种差异行为归因于ZAD的累积α-后坐损伤高出20% (3.34 × 1016衰变/g vs. 2.67 × 1016衰变/g),即使在预退火处理后仍作为残余损伤存在。每原子位移(dpa)的计算进一步量化了这种差异(ZAD为1.07 × 10−3,ZPC为8.5 ×−4)。研究表明,辐射损伤在不同时间尺度上(ZAD为134 Ma, ZPC为80 Ma)的累积会产生不同的微观结构缺陷模式,显著影响裂变径迹退火动力学,这对锆石热年代学解释和地质热历史重建具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Physics and Chemistry of Minerals
Physics and Chemistry of Minerals 地学-材料科学:综合
CiteScore
2.90
自引率
14.30%
发文量
43
审稿时长
3 months
期刊介绍: Physics and Chemistry of Minerals is an international journal devoted to publishing articles and short communications of physical or chemical studies on minerals or solids related to minerals. The aim of the journal is to support competent interdisciplinary work in mineralogy and physics or chemistry. Particular emphasis is placed on applications of modern techniques or new theories and models to interpret atomic structures and physical or chemical properties of minerals. Some subjects of interest are: -Relationships between atomic structure and crystalline state (structures of various states, crystal energies, crystal growth, thermodynamic studies, phase transformations, solid solution, exsolution phenomena, etc.) -General solid state spectroscopy (ultraviolet, visible, infrared, Raman, ESCA, luminescence, X-ray, electron paramagnetic resonance, nuclear magnetic resonance, gamma ray resonance, etc.) -Experimental and theoretical analysis of chemical bonding in minerals (application of crystal field, molecular orbital, band theories, etc.) -Physical properties (magnetic, mechanical, electric, optical, thermodynamic, etc.) -Relations between thermal expansion, compressibility, elastic constants, and fundamental properties of atomic structure, particularly as applied to geophysical problems -Electron microscopy in support of physical and chemical studies -Computational methods in the study of the structure and properties of minerals -Mineral surfaces (experimental methods, structure and properties)
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