Short communication: Inverse correlation between radiation damage and fission-track etching time on monazite
-
Published:2024-07-03
Issue:3
Volume:6
Page:313-323
-
ISSN:2628-3719
-
Container-title:Geochronology
-
language:en
-
Short-container-title:Geochronology
Author:
Nakajima ToruORCID, Fukuda Shoma, Sueoka ShigeruORCID, Niki Sota, Kawakami Tetsuo, Danhara Tohru, Tagami Takahiro
Abstract
Abstract. In this study, we explored the impacts of radiation damage and chemical composition on the etching time of fission tracks in monazite. Despite the potential of monazite fission-track (MFT) dating as an ultralow-temperature thermochronology, the comprehensive effects of radiation damage and non-formula elements, especially on the etching rate of MFTs, remain unexplored, and established analytical procedures are lacking. We quantified the degree of radiation damage (ΔFHWM) in Cretaceous to Quaternary monazites distributed in the Japan arc through Raman spectroscopy and chemical composition analyses. Subsequently, MFT etching was performed to examine the correlation between these parameters and the etching time. Estimation of the degree of radiation damage showed an increase in radiation damage corresponding to the cooling age of each geological unit. For example, the Toya ignimbrite (ca. 0.1 Ma) and the Kurobegawa granodiorite (< 0.8 Ma), both of which are types of monazite from Quaternary geological units, have ΔFHWM values of 0.27 and 0.55 cm−1, respectively. In contrast, the Muro ignimbrite (ca. 15 Ma) has a ΔFHWM value of 4.01 cm−1, while the Kibe granite and the Sagawa granite, both of which are Cretaceous granitoids, yielded 7.35 and 6.31 cm−1, respectively. MFT etching of these samples according to the existing recipe (6 M HCl at 90 °C for 60–90 min) was completed at 1200, 860, 210, 120, and 90 min for the Toya ignimbrite, Kurobegawa granodiorite, Muro ignimbrite, Sagawa granite, and Kibe granite, respectively. These outcomes highlight an inverse relationship between MFT etching time and the degree of radiation damage in monazite, while the correlation between MFT etching time and chemical composition was unclear. The results affirm earlier considerations that the etching rate of MFTs is strongly influenced by radiation damage. Conversely, young samples with lower levels of radiation damage exhibit higher chemical resistance, suggesting that existing etching recipes may not adequately etch MFTs.
Funder
Ministry of Economy, Trade and Industry
Publisher
Copernicus GmbH
Reference44 articles.
1. Burtner, R. L., Nigrini, A., and Donelick, R. A.: Thermochronology of Lower Cretaceous Source Rocks in the Idaho-Wyoming Thrust Belt, Am. Assoc. Pet. Geol. Bull., 78, 1613–1636, https://doi.org/10.1306/A25FF233-171B-11D7-8645000102C1865D, 1994. 2. Fayon, A. K.: Fission Track Dating of Monazite: Etching Efficiencies as a Function of U Content, in: GSA Annual Meeting, Geological Society of America, Minneapolis, p. 331, 2011. 3. Fleischer, R. L. and Price, P. B.: Techniques for geological dating of minerals by chemical etching of fission fragment tracks, Geochim. Cosmochim. Ac., 28, 1705–1714, https://doi.org/10.1016/0016-7037(64)90017-1, 1964. 4. Gleadow, A. J. W., Hurford, A. J., and Quaife, R. D.: Fission track dating of zircon: Improved etching techniques, Earth Planet. Sc. Lett., 33, 273–276, https://doi.org/10.1016/0012-821X(76)90235-1, 1976. 5. Goto, Y., Suzuki, I, K., Shinya, T., Yamauchi, I., A., Miyoshi, M., Danhara, T., and Tomiya, A.: Stratigraphy and Lithofacies of the Toya Ignimbrite in Southwestern Hokkaido, Japan: Insights into the Caldera-forming Eruption at Toya Caldera, J. Geogr. (Chigaku Zasshi), 127, 191–227, https://doi.org/10.5026/jgeography.127.191, 2018.
|
|