A revised alpha-ejection correction calculation for (U–Th) ∕ He thermochronology dates of broken apatite crystals

IF 2.7 Q2 GEOCHEMISTRY & GEOPHYSICS Geochronology Pub Date : 2022-10-27 DOI:10.5194/gchron-4-629-2022
John He, P. Reiners
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引用次数: 1

Abstract

Abstract. Accurate corrections for the effects of alpha ejection (the loss of daughter He near grain or crystal surfaces due to long alpha stopping distances) are central to (U-Th)/He thermochronometry. In the case of apatite (U-Th)/He dating, alpha-ejection correction is complicated by the fact that crystals are often broken perpendicular to the c axis. In such cases, the correction should account for the fact that only some parts of the crystal are affected by alpha ejection. A common current practice to account for such broken crystals is to modify measured lengths of broken crystals missing one termination by a factor of 1.5, and those missing both terminations by a factor of 2. This alpha-ejection “correction correction” systematically overestimates the actual fraction of helium lost to alpha ejection, and thus overcorrects the measured date relative to that determined for an otherwise equivalent unbroken crystal. The ratio of the alpha-ejection-affected surface area to the volume of a fragmented crystal is equivalent to the surface-area-to-volume ratio of an unbroken crystal that is either twice as long (for fragments with one termination) or infinitely long (for fragments with no termination). We suggest that it is appropriate to revise the fragmentation correction to multiply the lengths of crystals missing one c-axis termination by 2, and those missing both c-axis terminations by some large number ≳20. We examine the effect of this revised correction and demonstrate the accuracy of the new method using synthetic datasets. Taking into account alpha ejection, the rounding of the He concentration profile due to diffusive loss, and the accumulation of radiation damage over a range of thermal histories, we show that the revised fragmentation alpha-ejection correction proposed here accurately approximates the corrected date of an unbroken crystal (“true” date) to within <0.7 % on average (±4.2 %, 1σ), whereas the former method overcorrects dates to be ∼3 % older than the “true” date on average. For individual grains, the former method can result in dates that are older by a few percent in most cases, and by as much as 12 % for grains with aspect ratios of up to 1:1. The revised alpha-ejection correction proposed here is both more accurate and more precise than the previous correction, and does not introduce any significant systematic bias into the apparent dates from a sample.
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破碎磷灰石晶体(U-Th)∕He热年代学的α -喷射修正计算
摘要对α喷射效应(由于α停止距离较长而在晶粒或晶体表面附近损失子He)的精确校正是(U-Th)/He热时计的核心。在磷灰石(U-Th)/He测年的情况下,由于晶体经常垂直于c轴破碎,α喷射校正变得复杂。在这种情况下,修正应考虑到只有晶体的某些部分受到α喷射的影响。一种常见的目前的做法来解释这种破碎的晶体是修改破碎晶体的测量长度,其中一个端缺失1.5倍,两个端缺失2倍。这种α喷射“修正修正”系统地高估了α喷射所损失的氦的实际比例,因此相对于其他等效的未破碎晶体所确定的测量日期,高估了测量日期。弹射影响的表面积与破碎晶体体积之比相当于未破碎晶体的表面积与体积之比,而未破碎晶体的长度要么是两倍(对于有一端的碎片),要么是无限长(对于没有一端的碎片)。我们建议适当地修正碎片修正,将缺少一个c轴末端的晶体长度乘以2,而同时缺少两个c轴末端的晶体长度乘以较大的数(约20)。我们检验了这种修正的影响,并证明了使用合成数据集的新方法的准确性。考虑到α抛射,由于扩散损失导致的He浓度曲线的舍入,以及在热历史范围内辐射损伤的累积,我们表明,这里提出的修正碎片α抛射校正准确地接近未破碎晶体的校正日期(“真实”日期)平均在< 0.7%(±4.2%,1σ)以内,而前一种方法将日期过度校正,平均比“真实”日期老约3%。对于单个谷物,前一种方法在大多数情况下会导致日期变老几个百分点,对于长径比高达1:1的谷物,可能会导致日期变老12%。本文提出的修正α -抛射校正比以前的校正更准确,更精确,并且不会对样本的表观日期引入任何显著的系统偏差。
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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