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Showing 1–8 of 8 results
Advanced filters: Author: Kenneth C. Creager Clear advanced filters

  • Slow slip of the down-going plate at subduction zones can generate seismic tremor. Analysis of recent large tremor and slip episodes along the Cascadia subduction zone reveals tremor signals that reverse and rapidly migrate back along the previously ruptured fault, implying that the initial fault slip weakened the plate interface.

    • Heidi Houston
    • Brent G. Delbridge
    • Kenneth C. Creager
    Research
    Nature Geoscience
    Volume: 4, P: 404-409

  • Movement of the down-going oceanic plate in subduction zones is accommodated by earthquakes, slow slip and free slip with increasing depth. Analysis of accompanying tremor reveals a continuum of slow-slip events in the Cascadia subduction zone, which suggests that deep free slip of the subducted plate may cause stress to be gradually transferred up the plate interface towards the seismogenic zone.

    • Aaron G. Wech
    • Kenneth C. Creager
    Research
    Nature Geoscience
    Volume: 4, P: 624-628

  • Different measurements of inner core rotation have delivered inconsistent results. An analysis of seismic data provides a resolution of this discrepancy by suggesting decadal variations in inner core rotation rate.

    • Kenneth C. Creager
    News & Views
    Nature Geoscience
    Volume: 6, P: 424-426

  • The indications are that a solid ball of iron lies at Earth's centre. But only the identification of an elusive seismic signature can confirm the long-standing assumption that it is indeed solid.

    • Kenneth C. Creager
    News & Views
    Nature
    Volume: 454, P: 833-835

  • Seismic data during the time interval between larger earthquakes could contain information about fault displacements and potential for future failure, suggest analyses of data from laboratory and real-world slow-slip earthquakes using machine-learning techniques.

    • Kenneth C. Creager
    News & Views
    Nature Geoscience
    Volume: 12, P: 5-6