Deconvolution of fission-track length distributions and its application to dating and separating pre- and post-depositional components

IF 2.7 Q2 GEOCHEMISTRY & GEOPHYSICS
P. Jensen, K. Hansen
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引用次数: 0

Abstract

Abstract. To enable the separation of pre- and postdepositional components of the length distribution of (partially annealed) horizontal confined fission tracks, the length distribution is corrected by deconvolution. Probabilistic least-squares inversion corrects natural track length histograms for observational biases, considering the variance in data, modelization, and prior information. The corrected histogram is validated by its variance–covariance matrix. It is considered that horizontal track data can exist with or without measurements of angles to the c axis. In the latter case, 3D histograms are introduced as an alternative to histograms of c-axis-projected track lengths. Thermal history modelling of samples is not necessary for the calculation of track age distributions of corrected tracks. In an example, the age equations are applied to apatites with predepositional (inherited) tracks in order to extract the postdepositional track length histogram. Fission tracks generated before deposition in detrital apatite crystals are mixed with post-depositional tracks. This complicates the calculation of the post-sedimentary thermal history, as the grains have experienced different thermal histories prior to deposition. Thereafter, the grains share a common thermal history. Thus, the extracted post-depositional histogram without inherited tracks may be used for thermal history calculation.
裂变径迹长度分布的反褶积及其在沉积前后组分定年和分离中的应用
摘要为了分离(部分退火)水平受限裂变径迹长度分布的沉积前和沉积后成分,长度分布通过反褶积进行校正。考虑到数据、建模和先验信息的方差,概率最小二乘反演校正了观测偏差的自然轨迹长度直方图。校正后的直方图通过方差-协方差矩阵进行验证。认为水平轨迹数据可以存在与c轴的角度测量或不存在。在后一种情况下,引入3D直方图作为c轴投影轨迹长度直方图的替代方法。样品的热历史模拟对于计算修正径迹年龄分布是不必要的。在一个例子中,将年龄方程应用于具有沉积前(继承)径迹的磷灰石,以提取沉积后径迹长度直方图。碎屑磷灰石晶体沉积前的裂变径迹与沉积后的裂变径迹混合在一起。这使得沉积后热历史的计算变得复杂,因为颗粒在沉积前经历了不同的热历史。此后,这些颗粒具有共同的热历史。因此,提取的无遗传径迹的沉积后直方图可用于热历史计算。
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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