Published In

Journal of Geophysical Research: Solid Earth

Document Type

Article

Publication Date

10-6-2014

Subjects

Hikurangi Subduction Zone, Earthquake prediction, Earthquake hazard analysis -- New Zealand

Abstract

lnterseismic locking on the Hikurangi subduction zone in New Zealand is examined in light of alternative assumed locking distributions and the impact of transients (slow-slip and volcanic sources) on temporal and spatial resolution. The modern pattern of locking in the north is poorly resolved and, based on simulations of possible transient behavior, may be an ephemeral feature of the subduction cycle. While there appears to be some contemporary locking in the northern half of the Hikurangi subduction zone (HSZ), its location is model dependent, and hence, its relationship to structure, slow-slip, or any transition zone there is unclear. Simulations of site velocities using the 14 year history of transient events reveal that in the timescale of the interseismic period the northern half of the HSZ could be either locked or unlocked, and this may not be resolvable for decades. In the southern half, there is strong contemporary locking in the 15 to 40 km depth range, but again, the slow-slip history leads to uncertainty in the long-term pattern. Slow-slip events not only reduce the long-term locking by aseismic slip but also greatly hinder our ability to see it. It is within the range of possible models that the slip deficit rate at the HSZ is more uniform along strike, and the modern appearance is controlled by the particular pattern of transients over the past 10 to 20 years when the GPS data were collected. Similarly, uncertainties in surface velocities will be large at any subduction zone with large transients.

Description

This is the publisher's final pdf. Originally published in Journal of Geophysical Research: Solid Earth and is copyrighted by the American Geophysical Union.

Archived with permission.

DOI

10.1 002/2014JB01 0945

Persistent Identifier

http://archives.pdx.edu/ds/psu/13220

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