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Coseismic Gravity and Displacement Signatures Induced by the 2013 Okhotsk Mw8.3 Earthquake

Zhang, Guoqing, Shen, Wenbin, Xu, Changyi, and Zhu, Yiqing, 2016. Coseismic Gravity and Displacement Signatures Induced by the 2013 Okhotsk Mw8.3 Earthquake. Sensors, 16(9):1410, doi:10.3390/s16091410.

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BibTeX

@ARTICLE{2016Senso..16.1410Z,
       author = {{Zhang}, Guoqing and {Shen}, Wenbin and {Xu}, Changyi and {Zhu}, Yiqing},
        title = "{Coseismic Gravity and Displacement Signatures Induced by the 2013 Okhotsk Mw8.3 Earthquake}",
      journal = {Sensors},
     keywords = {Okhotsk Mw8.3 earthquake, GRACE, dislocation theory, coseismic gravity changes, coseismic displacements},
         year = 2016,
        month = sep,
       volume = {16},
       number = {9},
          eid = {1410},
        pages = {1410},
     abstract = "{In this study, Gravity Recovery and Climate Experiment (GRACE) RL05 data
        from January 2003 to October 2014 were used to extract the
        coseismic gravity changes induced by the 24 May 2013 Okhotsk
        Mw8.3 deep-focus earthquake using the difference and least
        square fitting methods. The gravity changes obtained from GRACE
        data agreed well with those from dislocation theory in both
        magnitude and spatial pattern. Positive and negative gravity
        changes appeared on both sides of the epicenter. The positive
        signature appeared on the western side, and the peak value was
        approximately 0.4 microgal (1 microgal = 10$^{-8}$ m/s$^{2}$),
        whereas on the eastern side, the gravity signature was negative,
        and the peak value was approximately -1.1 microgal. It
        demonstrates that deep-focus earthquakes Mw {\ensuremath{\leq}}
        8.5 are detectable by GRACE observations. Moreover, the
        coseismic displacements of 20 Global Positioning System (GPS)
        stations on the Earth's surface were simulated using an elastic
        dislocation theory in a spherical earth model, and the results
        are consistent with the GPS results, especially the near-field
        results. We also estimated the gravity contributions from the
        coseismic vertical displacements and density changes, analyzed
        the proportion of these two gravity change factors (based on an
        elastic dislocation theory in a spherical earth model) in this
        deep-focus earthquake. The gravity effect from vertical
        displacement is four times larger than that caused by density
        redistribution.}",
          doi = {10.3390/s16091410},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2016Senso..16.1410Z},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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