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Reconstruction of Nonlinear Geochemical Dynamics of Elemental Sedimentation Based on Power Spectral Analysis of Time Sequence

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Abstract

Maximum entropy spectral analysis and multidimensional cross-spectral analysis are two important tools for studying periodicity of elemental sedimentation in strata. They are applied to the study of the Devonian lensoid limestone formation in the Nandan-Hechi basin of Guangxi, China. Results show that all major element oxides of the sedimentary formation display a consistent change period of about 4 m; however, elements do not change in step. Nonlinear geochemical dynamic processes of elemental sedimentation through sea-floor fluids may be effectively reconstructed based on power spectral analyses.

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Zhou, Y. Reconstruction of Nonlinear Geochemical Dynamics of Elemental Sedimentation Based on Power Spectral Analysis of Time Sequence. Mathematical Geology 31, 723–742 (1999). https://doi.org/10.1023/A:1007584511667

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