Station misorientation inversion consistency
Seismometer rotation obtained when phase velocity structure is varied: expanding the phase velocity degree 16 or degree 20, and including just arrival angle data or both arrival angle and phase data (four symbols for each station).
Erik Larson
,
Department of Earth and Planetary Sciences
,
Harvard University
.
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Last modified: Thu Jan 29 09:16:34 EST
Seismometer rotation obtained when phase velocity structure is varied: expanding the phase velocity degree 16 or degree 20, and including just arrival angle data or both arrival angle and phase data (four symbols for each station).