Evaluating the coastal deformation mechanisms of the Raukumara Peninsula, northern Hikurangi subduction margin, New Zealand and insights into forearc uplift processes-Reference-Cited by-同舟云学术

Evaluating the coastal deformation mechanisms of the Raukumara Peninsula, northern Hikurangi subduction margin, New Zealand and insights into forearc uplift processes

Published:2010-12 Issue:4 Volume:53 Page:341-358
ISSN:0028-8306
Container-title:New Zealand Journal of Geology and Geophysics
language:en
Short-container-title:New Zealand Journal of Geology and Geophysics

Author:

Clark K,Berryman K,Litchfield N,Cochran U,Little T

Publisher

Informa UK Limited

Subject

Earth and Planetary Sciences (miscellaneous),Geology,Geophysics

Link

http://www.tandfonline.com/doi/pdf/10.1080/00288306.2010.520324

Reference89 articles.

1. Spatial and temporal strain rate variations at the northern Hikurangi margin, New Zealand

2. Evidence for Great Holocene Earthquakes Along the Outer Coast of Washington State

3. Formation of an active thrust triangle zone associated with structural inversion in a subduction setting, eastern New Zealand

4. Late Cenozoic evolution and earthquake potential of an active listric thrust complex above the Hikurangi subduction zone, New Zealand

5. Seismic reflection character of the Hikurangi subduction interface, New Zealand, in the region of repeated Gisborne slow slip events

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