Relative Sea‐Level Changes Over the Past Centuries in the Central Ryukyu Arc Inferred From Coral Microatolls-Reference-Cited by-同舟云学术

Relative Sea‐Level Changes Over the Past Centuries in the Central Ryukyu Arc Inferred From Coral Microatolls

Published:2020-02 Issue:2 Volume:125 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Weil‐Accardo J.¹²,Feuillet N.³,Satake K.²,Goto T.²,Goto K.⁴,Harada T.²,Kayanne H.⁵,Nakamura M.⁶,Ramos N.⁷,Saurel J.‐M.³,Sowa K.⁸,Liu S.‐C.⁹,Yu T.‐L.¹⁹¹⁰,Shen C.‐C.¹⁹¹⁰

Affiliation:

1. Now at CEREGEAix‐Marseille University Aix‐en Provence France

2. Earthquake Research InstituteUniversity of Tokyo Tokyo Japan

3. Institut de Physique du Globe de ParisSorbonne Paris University, Paris‐Diderot University, UMR 7154 Paris France

4. International Research Institute of Disaster ScienceTohoku University Sendai Japan

5. Department of Earth and Planetary ScienceUniversity of Tokyo Tokyo Japan

6. Faculty of ScienceUniversity of the Ryukyus Okinawa Japan

7. National Institute of Geological SciencesUniversity of the Philippines‐Diliman Quezon City Philippines

8. Japan Agency for Marine‐Earth Science and Technology Kanagawa Japan

9. Department of GeosciencesNational Taiwan University Taipei Taiwan ROC

10. Research Center for Future EarthNational Taiwan University Taipei Taiwan ROC

Funder

National Taiwan University

Publisher

American Geophysical Union (AGU)

Subject

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

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019JB018466

Reference112 articles.

1. Recent intensification of tropical climate variability in the Indian Ocean

2. Source of high tsunamis along the southernmost Ryukyu trench inferred from tsunami stratigraphy

3. Is the Ryukyu subduction zone in Japan coupled or decoupled? —The necessity of seafloor crustal deformation observation

4. Interseismic deformation at the Nankai subduction zone and the Median Tectonic Line, southwest Japan

5. High-density surveys conducted to reveal active deformations of the upper forearc slope along the Ryukyu Trench, western Pacific, Japan

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