4.5 Article

Clustering Analysis Methods for GNSS Observations: A Data-Driven Approach to Identifying California's Major Faults

Journal

EARTH AND SPACE SCIENCE
Volume 8, Issue 11, Pages -

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2021EA001680

Keywords

clustering; geodetic imaging; tectonics; GNSS; faults; earthquake

Funding

  1. NASA's ACCESS, Advanced Information Systems Technology (AIST)
  2. Earth Surface and Interior (ESI) programs
  3. Geodetic Imaging

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The data-driven approach presented in this study allows clustering of GNSS stations based on observed velocities, displacements, or other selected characteristics. The method provides valuable scientific information and is essential for further analysis. By selecting desired features of the data for clustering, the stations can be autonomously grouped using a selected clustering method.
We present a data-driven approach to clustering or grouping Global Navigation Satellite System (GNSS) stations according to observed velocities, displacements or other selected characteristics. Clustering GNSS stations provides useful scientific information, and is a necessary initial step in other analysis, such as detecting aseismic transient signals (Granat et al., 2013, https:// doi.org/10.1785/0220130039). Desired features of the data can be selected for clustering, including some subset of displacement or velocity components, uncertainty estimates, station location, and other relevant information. Based on those selections, the clustering procedure autonomously groups the GNSS stations according to a selected clustering method. We have implemented this approach as a Python application, allowing us to draw upon the full range of open source clustering methods available in Python's scikit-learn package (Pedregosa et al., 2011, https://doi.org/10.5555/1953048.2078195). The application returns the stations labeled by group as a table and color coded KML file and is designed to work with the GNSS information available from GeoGateway (Donnellan et al., 2021, https://doi.org/10.1007/ s12145-020-00561-7; Heflin et al., 2020, https://doi.org/10.1029/2019ea000644) but is easily extensible. We demonstrate the methodology on California and western Nevada. The results show partitions that follow faults or geologic boundaries, including for recent large earthquakes and post-seismic motion. The San Andreas fault system is most prominent, reflecting Pacific-North American plate boundary motion. Deformation reflected as class boundaries is distributed north and south of the central California creeping section. For most models a cluster boundary connects the southernmost San Andreas fault with the Eastern California Shear Zone (ECSZ) rather than continuing through the San Gorgonio Pass.

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