Figure 19.
Geoid anomaly for an inclined strike-slip fault computed on the free surface at 0, 100, 200 and 300 yr after the earthquake (top to bottom). Left column: SIEM using the moment-density tensor approach. Right column: SIEM using the split-node approach.

Geoid anomaly for an inclined strike-slip fault computed on the free surface at 0, 100, 200 and 300 yr after the earthquake (top to bottom). Left column: SIEM using the moment-density tensor approach. Right column: SIEM using the split-node approach.

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