The observed source properties of shallow SSEs in Hikurangi do not show a clear trend, which could be due to a limited range of durations and moments sampled by the shallow SSEs, as well as a short catalog ( < 20 yr).
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Segmentation of Shallow Slow Slip Events at the Hikurangi Subduction Zone Explained by Along-Strike Changes in Fault Geometry and Plate Convergence Rates.
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