日本地球惑星科学連合2019年大会

講演情報

[J] ポスター発表

セッション記号 M (領域外・複数領域) » M-GI 地球科学一般・情報地球科学

[M-GI33] データ駆動地球惑星科学

2019年5月27日(月) 17:15 〜 18:30 ポスター会場 (幕張メッセ国際展示場 8ホール)

コンビーナ:桑谷 立(国立研究開発法人 海洋研究開発機構)、長尾 大道(東京大学地震研究所)、上木 賢太(国立研究開発法人海洋研究開発機構)、加納 将行(東北大学理学研究科)

[MGI33-P02] Bayesian statistical evaluation method for detrital zircon geochronology

*古川 旦1辻森 樹1 (1.東北大学)

キーワード:ベイズ統計学、砕屑性ジルコン年代学、MCMCアルゴリズム

Over the past two decades, detrital zircon U-Pb geochronology has become an essential method not only in sedimentary provenance analyses but also in characterization of sedimentary and metamorphic strata. Although the age data has been conventionally evaluated by using relative frequency plots (here after called histograms) and density curves, the lack of statistical verification can cause miss reading of data. In order to overcome the statistical issues raised, this study proposes new statistical evaluation method for detrital zircon geochronology.
The new method is based on Bayesian statistics, adapted a theory proposed by Riihimäki and Vehtari (2014) that provides a flexible modeling for density curve using the Logistic Gaussian Process (LGP)
For introducing non-negative consistency for density curve, the logistic density transformation is performed by p(x)=exp(f(x))/∫exp(f(s))ds; x is age, p(x) is density curve, and f(x) is Gaussian Process; f(x)∼GP(0,κ(x,x')). The covariance matrix κ(x,x') is calculated by Gaussian kernel with hyperparameters ρ and σ. For the actual computation, the logistic density transformation has integral difficulties, then, M discretized softmax function is used for approximation for it.
The likelihood function is L(p|ρ,σ)=yTp. p is M discretized p(x), and y is vector of yi, which is the number of observations that fall within the i'th M discretized age subregion.
We have used programming language R and Stan for the MCMC computation of the statistical model above. When the number of detrital zircon data is several hundred or less, the hyperparameters of Gaussian process ρ and σ do not converge, and Bayesian estimation can not be performed. For this reason, the author estimated most plausible ρ and σ by WAIC. Using zircon data from our own data and the literature, in this presentation, we will demonstrate powerfulness of our new statistical evaluation.