Geological data such as the strike of bedding, paleocurrent direc-ions, paleomagnetic directions, and the trend of mineral lineations are directional data defined by an angle from a reference direction. The main characteristic of such data is circularity in any reference direction (i.e. 0°=360°), which creates problems when analyzing the data statistically. In this regard, only directional statistics are ade-quate for dealing with directional data. This paper introduces the fundamental theory of circular statistics, a form of directional statistics that is restricted to data on a circumference, and presents practical methods with which to analyze circular data, including their graphical representation, descriptive statistics, the characteristics of circular uniform and von Mises distributions, tests of goodness-of-fit, and single- and multi-sample statistical tests. In addition, statistical software is considered with which to analyze circular data.
CITATION STYLE
Arai, H. (2011). Circular statistics for the analysis of directional geological data. The Journal of the Geological Society of Japan, 117(10), 547–564. https://doi.org/10.5575/geosoc.117.547
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