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A Bayesian approach to calibrating apatite fission track annealing models for laboratory and geological timescales

机译:贝叶斯方法校准实验室和地质时标的磷灰石裂变径迹退火模型

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摘要

We present a new approach for modelling annealing of fission tracks in apatite, aiming to address various problems with existing models. We cast the model in a fully Bayesian context, which allows us explicitly to deal with data and parameter uncertainties and correlations, and also to deal with the predictive uncertainties. We focus on a well-known annealing algorithm [Laslett, G.M., Green, P.F., Duddy, I.R., Gleadow. A.J.W., 1987. Thermal annealing of fission tracks in apatite. 2. A quantitative-analysis. Chem. Geol., 65 (1), 1-13], and build a hierachical Bayesian model to incorporate both laboratory and geological timescale data as direct constraints. Relative to the original model calibration, we find a better (in terms of likelihood) model conditioned just on the reported laboratory data. We then include the uncertainty on the temperatures recorded during the laboratory annealing experiments. We again find a better model, but the predictive uncertainty when extrapolated to geological timescales is increased due to the uncertainty on the laboratory temperatures. Finally, we explictly include a data set [Vrolijk, P., Donelick, R.A., Quenq, J., Cloos. M., 1992. Testing models of fission track annealing in apatite in a simple thermal setting: site 800, leg 129. In: Larson, R., Lancelet, Y. (Eds.), Proceedings of the Ocean Drilling Program, Scientific Results, vol. 129, pp. 169-176] which provides low-temperature geological timescale constraints for the model calibration. When combined with the laboratory data, we find a model which satisfies both the low-temperature and high-temperature geological timescale benchmarks, although the fit to the original laboratory data is degraded. However, when extrapolated to geological timescales, this combined model significantly reduces the well-known rapid recent cooling artifact found in many published thermal models for geological samples. (c) 2006 Elsevier Inc. All rights reserved.
机译:我们提出了一种新的建模磷灰石裂变径迹退火的方法,旨在解决现有模型的各种问题。我们在完全贝叶斯的上下文中转换模型,这使我们可以显式地处理数据和参数的不确定性和相关性,还可以处理预测性的不确定性。我们专注于众所周知的退火算法[Laslett,G.M.,Green,P.F.,Duddy,I.R.,Gleadow。 A.J.W.,1987。磷灰石中裂变径迹的热退火。 2.定量分析。化学[Geol。,65(1),1-13],并建立一个多层次的贝叶斯模型,将实验室和地质时标数据都纳入直接约束条件。相对于原始模型校准,我们发现仅根据报告的实验室数据为基础的更好的模型(就可能性而言)。然后,我们将实验室退火实验期间记录的温度的不确定性包括在内。我们再次找到了一个更好的模型,但是由于实验室温度的不确定性,将其推算到地质时标时的预测不确定性增加了。最后,我们明确包含一个数据集[Vrolijk,P.,Donelick,R.A.,Quenq,J.,Cloos。 M.,1992。在简单的热环境下,在磷灰石中进行裂变径迹退火的测试模型:部位800,腿129。出处:Larson,R.,Lancelet,Y.(编辑),《海洋钻探计划》,科学结果,卷[第129页,第169-176页],为模型校准提供了低温地质时标约束。当与实验室数据结合时,尽管与原始实验室数据的拟合度降低了,但我们找到了一个满足低温和高温地质时标基准的模型。但是,如果将其外推至地质时标,则此组合模型将大大减少在许多已发布的地质样品热模型中发现的众所周知的快速近期冷却伪影。 (c)2006 Elsevier Inc.保留所有权利。

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