--- title: "Gonjo Demonstration" output: rmarkdown::html_vignette vignette: > %\VignetteIndexEntry{Gonjo Demonstration} %\VignetteEngine{knitr::rmarkdown} %\VignetteEncoding{UTF-8} --- ```{r, include = FALSE} knitr::opts_chunk$set( collapse = TRUE, comment = "#>" ) ``` ```{r setup} library(TFORGE) ``` The Gonjo basin anisotropy of magnetic susceptibility (AMS) data from Li et al. (2020) is available with the `TFORGE` package. This data contains the AMS tensor of 542 specimens along with the depth of each specimen. See `?Gonjo` for details. For analysis Li et al. (2020) split the data at depths of 765m and 2154m, leading to three intervals. Each AMS tensor is a 3 by 3 symmetric matrix with a trace of `1` and non-negative eigenvalues, so we can use `test_multiplicity_nonnegative()` and `test_fixedtrace()` to test some hypotheses relevant to AMS data. Because the eigenvalues of the matrices tend to be well away from zero (smallest eigenvalue of all matrices = 0.267), it would likely be okay to use `test_multiplicity()` too. Each interval has over 100 specimens. For fast computation in this demonstration we will use only the first 30 specimens of each interval, and only 100 bootstrap resamples. ## Preparation Split the AMS matrices in `Gonjo` into three groups, keeping the first 30 of each for computation speed in this demonstration. ```{r} interval_1 <- Gonjo$matrices[Gonjo$datatable$`really depth` <= 765] interval_2 <- Gonjo$matrices[Gonjo$datatable$`really depth` <= 2154] interval_3 <- Gonjo$matrices[Gonjo$datatable$`really depth` > 2154] samples <- list(`1` = interval_1[1:30], `2` = interval_2[1:30], `3` = interval_3[1:30]) ``` ## Multiplicity Tests Following descriptions from Li et al. (2020), here we will test whether population mean of intervals 1, 2, and 3 are oblate, isotropic, or prolate respectively. These are hypotheses about the multiplicity of eigenvalues of the population means. For interval 1 and 2 the samples are so far from oblate and isotropic, respectively, that weighted bootstrapping (using `emplik()`) could not be used, and the result is automatically a p-value of 0, corresponding to rejecting the null hypothesis. At a significance level of 0.05, the prolate hypothesis for interval 3 should also be rejected. Interval 1 oblate: ```{r} test_multiplicity_nonnegative(samples[["1"]], mult = c(2, 1), B = 1000) ``` Interval 2 isotropic: ```{r} test_multiplicity_nonnegative(samples[["2"]], mult = 3, B = 1000) ``` Interval 3 prolate: ```{r} test_multiplicity_nonnegative(samples[["3"]], mult = c(1, 2), B = 1000) ``` Because the eigenvalues of the data are so far away from zero (smallest eigenvalue of all matrices = 0.267) the transformation-based bootstrapping used by `test_multiplicity()` would likely work well too and give the same result. Below we apply `test_multiplicity()`, and the results lead to the same conclusions as `test_multiplicity_nonnegative()`. For computational speed in this demonstration we will use only 100 resamples; __we recommend using at least 1000 resamples in practise__. ```{r} test_multiplicity(samples[["1"]], mult = c(2, 1), B = 100) test_multiplicity(samples[["2"]], mult = 3, B = 100) test_multiplicity(samples[["3"]], mult = c(1, 2), B = 100) ``` ### 3-Sample Test Here we can check whether the eigenvalues of the population means are equal. Again the intervals are so different that the convex hulls of these samples do not overlap at the estimated common mean, so equality of eigenvalues is automatically rejected. ```{r} test_fixedtrace(samples, B = 1000) ``` ### Confidence Regions We can also estimate confidence regions for the eigenvalues of the population means. For computational speed in this demonstration we will use only 100 resamples; __we recommend using at least 1000 resamples in practise__. ```{r} s1_CR <- conf_fixedtrace(samples[["1"]], alpha = 0.05, B = 100, npts = 1000, check = FALSE ) s2_CR <- conf_fixedtrace(samples[["2"]], alpha = 0.05, B = 100, npts = 1000, check = FALSE ) s3_CR <- conf_fixedtrace(samples[["3"]], alpha = 0.05, B = 100, npts = 1000, check = FALSE ) ``` These confidence regions are ellipses on a 2D plane. Plotting these confidence regions can be a bit involved - please see the reproducibility documentation of Hingee et al. (2026) for an example using `ggplot2`. # References Li, S., van Hinsbergen, D. J. J., Shen, Z., Najman, Y., Deng, C., & Zhu, R. (2020). Anisotropy of Magnetic Susceptibility (AMS) Analysis of the Gonjo Basin as an Independent Constraint to Date Tibetan Shortening Pulses. *Geophysical Research Letters*, 47(8), e2020GL087531. https://doi.org/10.1029/2020GL087531 Hingee K, Scealy J, Wood A (2026). “Nonparametric bootstrap inference for the eigenvalues of geophysical tensors.” *Journal of American Statistical Association*. Accepted for publication.