Heterogeneous Sediment Input at the Nankai Trough Subduction Zone: Implications for Shallow Slow Earthquake Localization-Reference-Cited by-同舟云学术

Heterogeneous Sediment Input at the Nankai Trough Subduction Zone: Implications for Shallow Slow Earthquake Localization

Published:2021-10 Issue:10 Volume:22 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem Geophys Geosyst

Author:

Tilley H.¹^ORCID,Moore G. F.¹^ORCID,Underwood M. B.²^ORCID,Hernández‐Molina F. J.³,Yamashita M.⁴⁵,Kodaira S.⁴^ORCID,Nakanishi A.⁴^ORCID

Affiliation:

1. University of Hawai'i at Mānoa Honolulu HI USA

2. New Mexico Institute of Mining and Technology Socorro NM USA

3. Department of Earth Sciences Royal Holloway University of London Egham UK

4. Japan Agency for Marine‐Earth Science and Technology Yokohama Japan

5. National Institute of Advanced Industrial Science and Technology Geological Survey of Japan Ibaraki Japan

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GC009965

Reference150 articles.

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3. Seamount subduction erosion in the Nankai Trough and its potential impact on the seismogenic zone

4. Broad, weak regions of the Nankai Megathrust and implications for shallow coseismic slip

5. Geophysical Constraints on the Relationship Between Seamount Subduction, Slow Slip, and Tremor at the North Hikurangi Subduction Zone, New Zealand

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