Geology Department, University of Otago, Dunedin, New Zealand.
Institute of Earth Sciences, University of Iceland, Reykjavík, Iceland.
Sci Rep. 2020 Dec 10;10(1):21682. doi: 10.1038/s41598-020-78698-0.
Quantitative shape analysis of juvenile pyroclasts is applied in volcanology to reconstruct the dynamics and styles of eruptions, and to explore the details of tephra transport, dispersal, and emplacement. Morphometric analyses often include comparison of multiple data sets with a set of dimensionless shape parameters. Here we present "DendroScan", an open source Matlab program that provides the user with all the multivariate statistical methods needed to produce such morphometric comparisons. Serving as a statistical "toolbox", DendroScan conducts Levene-, t-, and equivalence tests, presenting the results in ad hoc interpretable graphs. Furthermore, it is designed to conduct dendrogrammatic analyses of particle morphometry, a recently developed approach for the inter-comparison of multiple morphometric data sets. DendroScan produces tree diagrams, in which the analysed samples are sorted according to their morphometric dissimilarity, allowing the user to identify, e.g., samples that are statistically equivalent. To demonstrate DendroScan's potential, ten experimental samples are compared with volcanic ash samples generated by the Havre 2012 deep-sea eruption in the Kermadec arc (New Zealand). We show how, using DendroScan-based results, information on the eruptive mechanism can be inferred, and how the cooling history of the experimental melt is reflected in the dissimilarity of thermally granulated fragments.
对幼年火山碎屑的定量形态分析被应用于火山学中,以重建喷发的动力学和喷发类型,并探索火山灰运移、扩散和堆积的细节。形态测量分析通常包括将多个数据集与一组无量纲形态参数进行比较。在这里,我们介绍了“DendroScan”,这是一个开源的 Matlab 程序,为用户提供了生成这种形态比较所需的所有多元统计方法。作为一个统计“工具箱”,DendroScan 进行 Levene、t 和等效性检验,并以专门可解释的图形呈现结果。此外,它还设计用于进行粒子形态测量的 dendrogrammatic 分析,这是一种最近开发的用于多个形态测量数据集比较的方法。DendroScan 生成树状图,其中根据形态差异对分析样本进行排序,允许用户识别例如在统计学上等效的样本。为了展示 DendroScan 的潜力,我们将十个实验样本与新喀里多尼亚克马德克弧(Kermadec arc)的 Havre 2012 深海喷发产生的火山灰样本进行了比较。我们展示了如何使用基于 DendroScan 的结果推断喷发机制的信息,以及实验熔体的冷却历史如何反映在热膨化碎片的差异中。