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Integrating CoDA and PCA for enhanced characterization of fluvial depositional processes: a case study of the Shendi formation, Sudan

  • Abdelrhim Eltijani*
  • , Musaab A.A. Mohammed
  • , Yousif Abuobida
  • , Ibrahim M. Yousif
  • *Corresponding author for this work

Research output: Contribution to journal › Article › peer-review

7 Scopus citations

Abstract

Traditional approaches to fluvial sedimentary analysis often face challenges in deciphering complex, multivariate datasets. This study combines compositional data analysis (CoDA) with principal component analysis (PCA) to enhance the characterization of depositional processes and sub-environments within the Shendi Formation. The PCA applied to centered log ratio (clr)-transformed grain size distributions, reveals three principal components with ~ 91.86% of the data variance explained, representing distinct processes: bedload-dominated channel-bar dynamics, overbank deposition, and high-energy flood events. Specific lithofacies associations strongly correlate to each principal component. This integrated approach enables the identification of subtle yet significant patterns within the complex sedimentological record. The Shendi Formation exhibits characteristics of a dynamic fluvial setting with variations in flow energy, channel migration, and periodic flooding. Our findings demonstrate the power of CoDA-PCA in refining the understanding of fluvial depositional systems and highlight its potential for broader applications.

Original languageEnglish
Article number10
JournalDiscover Geoscience
Volume2
Issue number1
DOIs
StatePublished - Dec 2024
Externally publishedYes

Bibliographical note

Publisher Copyright:
© The Author(s) 2024.

Keywords

  • Compositional data analysis (CoDA)
  • Fluvial deposition
  • Lithofacies associations
  • Principal component analysis (PCA)
  • Shendi Formation

ASJC Scopus subject areas

  • Earth and Planetary Sciences (miscellaneous)
  • Geology
  • Global and Planetary Change
  • Geophysics
  • Geochemistry and Petrology

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