4.7 Article

Estimation of Full Moment Tensors, Including Uncertainties, for Nuclear Explosions, Volcanic Events, and Earthquakes

Journal

JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
Volume 123, Issue 6, Pages 5099-5119

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2017JB015325

Keywords

seismic moment tensor; uncertainties; nuclear explosions; inverse problems; seismic source studies

Funding

  1. Air Force Research Laboratory [FA9453-15-C-0063, FA9453-17-C-0025]
  2. National Science Foundation [EAR-1215959]
  3. Swiss National Science Foundation [PP00P2 157627:OROG3NY]

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A seismic moment tensor is a 3 x 3 symmetric matrix that provides a compact representation of a seismic source. We develop an algorithm to estimate moment tensors and their uncertainties from observed seismic data. For a given event, the algorithm performs a grid search over the six-dimensional space of moment tensors by generating synthetic waveforms for each moment tensor and then evaluating a misfit function between the observed and synthetic waveforms. The moment tensor M-0 for the event is then the moment tensor with minimum misfit. To describe the uncertainty associated with M-0, we first convert the misfit function to a probability function. The uncertainty, or rather the confidence, is then given by the confidence curve (V), where (V) is the probability that the true moment tensor for the event lies within a certain neighborhood of M that has fractional volumeV. The area under the confidence curve provides a single, abbreviated confidence parameter for M-0. We apply the method to data from events in different regions and tectonic settings: 17 nuclear explosions and 12 earthquakes at the Nevada Test Site, 63 small (M-w<2.5) events at Uturuncu volcano in Bolivia, and 21 moderate (M-w>4) earthquakes in the southern Alaska subduction zone. Characterization of moment tensor uncertainties puts us in better position to discriminate among moment tensor source types and to assign physical processes to the events.

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