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      Time-scale and mechanism of subsidence at Lassen Volcanic Center, CA, from InSAR

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      Journal of Volcanology and Geothermal Research
      Elsevier BV

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          Synthetic aperture radar interferometry

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            Satellite radar interferometry: Two-dimensional phase unwrapping

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              Seismicity remotely triggered by the magnitude 7.3 landers, california, earthquake.

              The magnitude 7.3 Landers earthquake of 28 June 1992 triggered a remarkably sudden and widespread increase in earthquake activity across much of the western United States. The triggered earthquakes, which occurred at distances up to 1250 kilometers (17 source dimensions) from the Landers mainshock, were confined to areas of persistent seismicity and strike-slip to normal faulting. Many of the triggered areas also are sites of geothermal and recent volcanic activity. Static stress changes calculated for elastic models of the earthquake appear to be too small to have caused the triggering. The most promising explanations involve nonlinear interactions between large dynamic strains accompanying seismic waves from the mainshock and crustal fluids (perhaps including crustal magma).
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                Author and article information

                Journal
                Journal of Volcanology and Geothermal Research
                Journal of Volcanology and Geothermal Research
                Elsevier BV
                03770273
                June 2016
                June 2016
                : 320
                :
                : 117-127
                Article
                10.1016/j.jvolgeores.2016.04.013
                d75676f0-fc45-4c9e-aecd-83db61b5bf76
                © 2016
                History

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