反冲
白长石
微探针
离子
分析化学(期刊)
穿透深度
材料科学
矿物学
原子物理学
化学
物理
光学
核物理学
有机化学
色谱法
锆石
作者
W J Davis,Donald W. Davis
出处
期刊:Geophysical monograph
日期:2017-12-01
卷期号:: 247-259
被引量:21
标识
DOI:10.1002/9781119227250.ch11
摘要
206Pb/238U ratios have been measured as a function of depth beneath natural surfaces of baddeleyite crystals using a sensitive high-resolution ion microprobe (SHRIMP II). The data are compared to model profiles calculated using a stochastic averaging algorithm to constrain the average alpha recoil distance in baddeleyite. The precision of measured profiles is hampered by relatively high common Pb corrections near the surface and difficulty in estimating penetration depth at the start of measurements. Uncertainties in U concentration gradients within the first 200 nm may also influence the model profiles. Despite these difficulties, the measured U-Pb depth profiles are consistent with an alpha recoil distance in baddeleyite of 24 ± 7 nm. Assuming this recoil distance, Pb loss from near-surface alpha recoil becomes analytically resolvable for tabular crystals with thickness of <15–20 µm. This will not significantly affect ages based on 207Pb/206Pb ratios, but 206Pb/238U ages of bulk crystals may require corrections of 0.1–0.5% depending of grain size and shape. For typical tabular crystals, alpha recoil loss is linearly correlated with surface-area-to-volume ratios allowing simple corrections to be applied if the dimensions of the crystal are accurately determined prior to analyses.
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