Research Article| November 01, 2013 Revised Interface Geometry for the Hikurangi Subduction Zone, New Zealand Charles A. Williams; Charles A. Williams GNS Science, 1 Fairway Drive, Avalon, P.O. Box 30368, Lower Hutt 5040, New Zealand, U.S.A.c.williams@gns.cri.nz Search for other works by this author on: GSW Google Scholar Donna Eberhart‐Phillips; Donna Eberhart‐Phillips GNS Science, 1 Fairway Drive, Avalon, P.O. Box 30368, Lower Hutt 5040, New Zealand, U.S.A.c.williams@gns.cri.nz Search for other works by this author on: GSW Google Scholar Stephen Bannister; Stephen Bannister GNS Science, 1 Fairway Drive, Avalon, P.O. Box 30368, Lower Hutt 5040, New Zealand, U.S.A.c.williams@gns.cri.nz Search for other works by this author on: GSW Google Scholar Daniel H. N. Barker; Daniel H. N. Barker GNS Science, 1 Fairway Drive, Avalon, P.O. Box 30368, Lower Hutt 5040, New Zealand, U.S.A.c.williams@gns.cri.nz Search for other works by this author on: GSW Google Scholar Stuart Henrys; Stuart Henrys GNS Science, 1 Fairway Drive, Avalon, P.O. Box 30368, Lower Hutt 5040, New Zealand, U.S.A.c.williams@gns.cri.nz Search for other works by this author on: GSW Google Scholar Martin Reyners; Martin Reyners GNS Science, 1 Fairway Drive, Avalon, P.O. Box 30368, Lower Hutt 5040, New Zealand, U.S.A.c.williams@gns.cri.nz Search for other works by this author on: GSW Google Scholar Rupert Sutherland Rupert Sutherland GNS Science, 1 Fairway Drive, Avalon, P.O. Box 30368, Lower Hutt 5040, New Zealand, U.S.A.c.williams@gns.cri.nz Search for other works by this author on: GSW Google Scholar Seismological Research Letters (2013) 84 (6): 1066–1073. https://doi.org/10.1785/0220130035 Article history first online: 14 Jul 2017 Cite View This Citation Add to Citation Manager Share Icon Share MailTo Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Charles A. Williams, Donna Eberhart‐Phillips, Stephen Bannister, Daniel H. N. Barker, Stuart Henrys, Martin Reyners, Rupert Sutherland; Revised Interface Geometry for the Hikurangi Subduction Zone, New Zealand. Seismological Research Letters 2013;; 84 (6): 1066–1073. doi: https://doi.org/10.1785/0220130035 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietySeismological Research Letters Search Advanced Search The Hikurangi subduction zone extends along the eastern North Island of New Zealand southward into the northern portion of the South Island. It has drawn considerable recent attention due to the potential for large and/or tsunamigenic earthquakes, and both shallow and deep slow slip events (SSEs), as discussed in the next section. With such a wide range of seismic and aseismic behavior, the Hikurangi margin is an ideal natural laboratory for testing various types of subduction zone models. Furthermore, the possibility of a devastating megathrust earthquake also requires the development of models to evaluate the potential damage caused by such... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.