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New evidence from hybrid ground–based gravity observations of a regional gravity increase in southern Tibet before 2015

Jia, Lulu, Chen, Shi, Wang, Linhai, Lu, Hongyan, Liu, Mian, Xu, Weimin, He, Zhitang, Chen, Zhaohui, and Han, Jiancheng, 2026. New evidence from hybrid ground–based gravity observations of a regional gravity increase in southern Tibet before 2015. Tectonophysics, 925:231096, doi:10.1016/j.tecto.2026.231096.

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@ARTICLE{2026Tectp.92531096J,
       author = {{Jia}, Lulu and {Chen}, Shi and {Wang}, Linhai and {Lu}, Hongyan and {Liu}, Mian and {Xu}, Weimin and {He}, Zhitang and {Chen}, Zhaohui and {Han}, Jiancheng},
        title = "{New evidence from hybrid ground-based gravity observations of a regional gravity increase in southern Tibet before 2015}",
      journal = {Tectonophysics},
     keywords = {Nepal earthquake, Temporal gravity variation, Hybrid ground-based gravimetry, Surficial factors in gravity change},
         year = 2026,
        month = mar,
       volume = {925},
          eid = {231096},
        pages = {231096},
     abstract = "{The 2015 Mw 7.8 Nepal earthquake occurred in the Himalayan tectonic
        belt, where the Indian Plate collides with the Tibetan Plateau.
        High-precision ground gravimetry can be used to detect transient
        deep mass changes before the earthquake but limited by sparse
        absolute gravity stations and the effects of complex surficial
        factors. In this study, we present new evidence from hybrid
        terrestrial gravity measurements, carried out in southern Tibet
        near the epicenter of the 2015 Nepal earthquake. Measurements
        from 9 relative and 3 absolute gravity stations are integrated
        using a novel adjustment method. The results confirm the
        significant regional gravity increase before the 2015 Nepal
        earthquake, with a rate of about or larger than 15
        {\ensuremath{\mu}}Gal/yr (1 {\ensuremath{\mu}}Gal =
        10$^{{\ensuremath{-}}8}$ m/s$^{2}$) at four stations during
        2010─2013. We show that this gravity increase cannot be
        explained by vertical ground motion and/or local hydrological
        processes. Furthermore, due to inadequate spatial resolution,
        the observed gravity change could not be detected by the Gravity
        Recovery and Climate Experiment (GRACE) measurements. We suggest
        that the gravity increase could be caused by preseismic strain
        and mass (fluid) transfer in a broad seismogenic source region
        north of the Main Frontal Thrust. Absolute gravity observations
        show that the gravity increase stopped after the 2015 Nepal
        earthquake. Our results contribute to the exploration of
        possible precursors of large continental earthquakes and shed
        light on the potential mechanisms of large earthquakes in the
        Indo-Asian collision zone.}",
          doi = {10.1016/j.tecto.2026.231096},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2026Tectp.92531096J},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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