Exposure dating of detrital magnetite using 3He enabled by microCT and calibration of the cosmogenic 3He production rate in magnetite

IF 2.7 Q2 GEOCHEMISTRY & GEOPHYSICS Geochronology Pub Date : 2021-04-01 DOI:10.5194/GCHRON-3-395-2021
F. Hofmann, E. Cooperdock, A. West, Dominic Hildebrandt, Kathrin Strößner, K. Farley
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引用次数: 3

Abstract

Abstract. We test whether X-ray micro computed tomography (microCT) imaging can be used as a tool for screening magnetite grains to improve the accuracy and precision of cosmogenic 3He exposure dating. We extracted magnetite from a soil developed on a fanglomerate at Whitewater, California, which was offset by the Banning Strand of the San Andreas Fault. This study shows that microCT screening can distinguish between inclusion-free magnetite and magnetite with fluid or common solid inclusions. Such inclusions can produce bulk 3He concentrations that are significantly in excess of expected cosmogenic production. We present Li concentrations, major and trace element analysis, and magnetite (U-Th)/He cooling ages of samples in order to model the contribution from radiogenic, nucleogenic, and cosmogenic thermal neutron production of 3He. We show that mineral inclusions in magnetite can produce 3He concentrations of up to four times that of the cosmogenic 3He component, leading to erroneous exposure ages. Therefore, grains with inclusions must be avoided in order to facilitate accurate and precise magnetite 3He exposure dating. Around 30 % of all grains were found to be without inclusions, as detectable by microCT, with the largest proportion of suitable grains in the grain size range of 400–800 µm. While grains with inclusions have 3He concentrations far in excess of the values expected from existing 10Be and 26Al data in quartz at the Whitewater site, magnetite grains without inclusions have concentrations close to the predicted depth profile. We measured 3He concentrations in aliquots without inclusions and corrected them for Li-produced components. By comparing these data to the known exposure age of 53.5 ka, we calibrate a magnetite 3He SLHL production rate of 116 ± 13 at g−1 a−1. We suggest that the microCT screening approach can be used to improve the quality of cosmogenic 3He measurements of magnetite and other opaque mineral phases for exposure age and detrital studies.
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利用微ct技术对碎屑磁铁矿进行3He暴露定年,并对磁铁矿中宇宙成因3He产率进行校准
摘要我们测试了x射线微计算机断层扫描(microCT)成像是否可以作为筛选磁铁矿颗粒的工具,以提高宇宙起源3He暴露定年的准确性和精度。我们从加利福尼亚怀特沃特的一块尖砾岩上的土壤中提取了磁铁矿,这块土壤被圣安德烈亚斯断层的班宁线所抵消。本研究表明,微ct筛查可以区分无包裹体磁铁矿和含流体或常见固体包裹体的磁铁矿。这些包裹体可以产生大量的3He浓度,大大超过预期的宇宙成因产量。我们介绍了样品的Li浓度、主要元素和微量元素分析以及磁铁矿(U-Th)/He冷却年龄,以模拟放射成因、核成因和宇宙成因热中子产生3He的贡献。我们发现,磁铁矿中的矿物包裹体可以产生高达宇宙成因3He成分四倍的3He浓度,导致错误的暴露年龄。因此,必须避免含有包裹体的颗粒,以便准确和精确地确定磁铁矿3He暴露年代。通过显微ct检测发现,约30%的晶粒没有夹杂物,在400-800µm的晶粒尺寸范围内,合适晶粒的比例最大。虽然含有包裹体的颗粒的3He浓度远远超过了现有石英10Be和26Al数据的预期值,但没有包裹体的磁铁矿颗粒的浓度接近预测深度剖面。我们测量了不含包裹体的等分液中的3He浓度,并对其进行了锂生成成分的校正。通过将这些数据与已知的53.5 ka暴露年龄进行比较,我们校准了磁铁矿3He SLHL在g−1 a−1下的产率为116±13。我们建议,微ct筛选方法可用于提高宇宙成因3He测量磁铁矿和其他不透明矿物相的质量,用于暴露年龄和碎屑研究。
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
Geochronology
Geochronology Earth and Planetary Sciences-Paleontology
CiteScore
6.60
自引率
0.00%
发文量
35
审稿时长
19 weeks
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