The Hikurangi subduction zone - HazardsEducation.org

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Kapiti 2008 slow slip event lasted ~15 months, wasequivalent to a Magnitude 7.0 earthquakeWellingtonGNS Science
Slow slip events delineate the <strong>zone</strong> of locking on the<strong>subduction</strong> interfaceFault locking using campaign GPSvelocities averaged over the last~15 yearsGreen contours show total slip onthe interface in slow slip eventssince 2002Wallace and Beavan, in pressGNS Science
Page 1 and 2: The Hikurangi subduction zone: the
Page 3 and 4: New Zealand’sshaky situationbetwe
Page 5 and 6: Earthquakes in the North Island (19
Page 7 and 8: How do we unlock the secrets of the
Page 9 and 10: “Slow slip events” occur on the
Page 11 and 12: Examples of slow slip events(SSEs)
Page 13 and 14: SSEs in theHawke’sBay regionJune
Page 15: Total slip in the Kapiti 2003 and M
Page 19 and 20: Searching for pre-historic Subducti
Page 21 and 22: Hikurangi subduction interface eart
Page 23 and 24: Our latest understanding of the sub
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The Hikurangi subduction zone - HazardsEducation.org

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