Coupled afterslip and transient mantle flow after the 2011 Tohoku earthquake-Reference-Cited by-同舟云学术

Coupled afterslip and transient mantle flow after the 2011 Tohoku earthquake

Author:

Muto J.¹^ORCID,Moore J. D. P.²^ORCID,Barbot S.²³^ORCID,Iinuma T.⁴^ORCID,Ohta Y.⁵^ORCID,Iwamori H.⁶⁷⁸^ORCID

Affiliation:

1. Department of Earth Science, Tohoku University, Sendai, Japan.

2. Earth Observatory of Singapore, Nanyang Technological University, Singapore, Singapore.

3. Department of Earth Sciences, University of Southern California, Los Angeles, CA, USA.

4. Japan Agency for Marine-Earth Science and Technology, Yokohama, Japan.

5. Department of Geophysics, Tohoku University, Sendai, Japan.

6. Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan.

7. Earthquake Research Institute, The University of Tokyo, Tokyo, Japan.

8. Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Tokyo, Japan.

Abstract

Crustal deformation after the 2011 Tohoku earthquake illuminates the complex interplay between transient mantle flow and afterslip.

Funder

Japan Society for the Promotion of Science London

Japan Society for the Promotion of Science

Singapore Ministry of Education

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference55 articles.

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