Three‐Dimensional P Wave Velocity Structure of the Northern Hikurangi Margin From the NZ3D Experiment: Evidence for Fault‐Bound Anisotropy-Reference-Cited by-同舟云学术

Three‐Dimensional P Wave Velocity Structure of the Northern Hikurangi Margin From the NZ3D Experiment: Evidence for Fault‐Bound Anisotropy

Published:2020-11-26 Issue:12 Volume:125 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Arai Ryuta¹^ORCID,Kodaira Shuichi¹^ORCID,Henrys Stuart²^ORCID,Bangs Nathan³^ORCID,Obana Koichiro¹,Fujie Gou¹^ORCID,Miura Seiichi¹,Barker Daniel²^ORCID,Bassett Dan²,Bell Rebecca⁴,Mochizuki Kimihiro⁵^ORCID,Kellett Richard²^ORCID,Stucker Valerie²^ORCID,Fry Bill²,

Affiliation:

1. Research Institute for Marine Geodynamics Japan Agency for Marine‐Earth Science and Technology (JAMSTEC) Yokohama Japan

2. GNS Science Lower Hutt New Zealand

3. Institute for Geophysics University of Texas at Austin Austin TX USA

4. Imperial College London London UK

5. Earthquake Research Institute University of Tokyo Tokyo Japan

Funder

Japan Society for the Promotion of Science

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics