SAHKE geophysical transect reveals crustal and subduction zone structure at the southern Hikurangi margin, New Zealand-Reference-Cited by-同舟云学术

SAHKE geophysical transect reveals crustal and subduction zone structure at the southern Hikurangi margin, New Zealand

Published:2013-07 Issue:7 Volume:14 Page:2063-2083
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Henrys S.¹,Wech A.²,Sutherland R.¹,Stern T.²,Savage M.²,Sato H.³,Mochizuki K.³,Iwasaki T.³,Okaya D.⁴,Seward A.¹,Tozer B.⁵,Townend J.⁵,Kurashimo E.³,Iidaka T.³,Ishiyama T.³

Affiliation:

1. GNS Science; P.O. Box 30368 Lower Hutt 5040 New Zealand

2. SGEES; Victoria University of Wellington; Wellington New Zealand

3. Earthquake Research Institute, University of Tokyo; Tokyo Japan

4. Department of Earth Sciences; University of Southern California; Los Angeles California USA

5. SGEES; Victoria University of Wellington; New Zealand

Funder

Government of New Zealand, the Japanese Science and Technology Agency

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

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