Japan Geoscience Union Meeting 2023

Presentation information

[J] Online Poster

M (Multidisciplinary and Interdisciplinary) » M-GI General Geosciences, Information Geosciences & Simulations

[M-GI29] Data-driven geosciences

Mon. May 22, 2023 9:00 AM - 10:30 AM Online Poster Zoom Room (3) (Online Poster)

convener:Tatsu Kuwatani(Japan Agency for Marine-Earth Science and Technology), Hiromichi Nagao(Earthquake Research Institute, The University of Tokyo), Kenta Ueki(Japan Agency for Marine-Earth Science and Technology), Shin-ichi Ito(The University of Tokyo)

On-site poster schedule(2023/5/21 17:15-18:45)

9:00 AM - 10:30 AM

[MGI29-P02] Application of compositional data analysis to trace elements in clinopyroxene from abyssal peridotites

*Ikuya Nishio1,2, Keita Itano3, Pedro Waterton2, Akihiro Tamura1, Kristoffer Szilas2, Tomoaki Morishita1 (1.Kanazawa University, 2.University of Copenhagen, 3.Akita University)

Keywords:Clinopyroxene, Mantle, Peridotite, Statistical analysis

Data analysis using statistical and machine learning methods has recently been applied to geochemical data (Itano et al., 2020). We newly applied compositional data analysis (CoDA), including log-ratio transformation, principal component analysis, and k-means clustering on a large database of abyssal peridotite clinopyroxene composition and showed great potential for understanding compositional systematics (Nishio et al., 2022).
CoDA is a set of multivariate statistical analyses and is used for major element data (Aitchison, 1982). Compositional data consist of a matrix of nonnegative, relative values with a constant. In the Earth sciences, mineral chemical compositions are compositional data, and mineral trace element compositions are the parts of compositional data which is called subcomposition. Concentrations of various elements within a mineral are dependent on the concentrations of other elements in the mineral because the compositional data has a constant sum. Therefore, n-dimensional data are plotted on an nāˆ’1 dimensional space, as the concentration of one element is not an independent variable, and the potential for pseudo-correlations should be considered. CoDA considers and removes these constant-sum constraints on the following statistical analyses. We applied these methods to clinopyroxene trace element compositions, which are subcompositional data. In this presentation, we will introduce the analyses, performed by Nishio et al. (2022) and discuss the importance of log-ratio transformations in the statistical analysis of clinopyroxene trace elements.

References
Itano, K., Ueki, K., Iizuka, T., & Kuwatani, T. (2020). Geochemical discrimination of Monazite source rock based on machine learning techniques and multinomial logistic regression analysis. Geosciences, 10(2), 63. https://doi.org/10.3390/geosciences10020063
Nishio, I., Itano, K., Waterton, P., Tamura, A., Szilas, K., & Morishita, T. (2022). Compositional Data Analysis (CoDA) of Clinopyroxene From Abyssal Peridotites. Geochemistry, Geophysics, Geosystems, 23(8), e2022GC010472. https://doi.org/10.1029/2022GC010472
Aitchison, J. (1982). The statistical analysis of compositional data. Journal of the Royal Statistical Society: Series B, 44(2), 139ā€“ 160. https://doi.org/10.1111/J.2517-6161.1982.TB01195.X