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A combination of tides and nontidal variations in ocean bottom pressure may generate interannual slip fluctuations in the transition zone along a subduction plate interface

Yoshiyuki Tanaka Hiromu Sakaue Masayuki Kano Suguru Yabe

大地测量与地球动力学(英文版)2023,Vol.14Issue(1):43-51,9.
大地测量与地球动力学(英文版)2023,Vol.14Issue(1):43-51,9.

A combination of tides and nontidal variations in ocean bottom pressure may generate interannual slip fluctuations in the transition zone along a subduction plate interface

A combination of tides and nontidal variations in ocean bottom pressure may generate interannual slip fluctuations in the transition zone along a subduction plate interface

Yoshiyuki Tanaka 1Hiromu Sakaue 1Masayuki Kano 2Suguru Yabe3

作者信息

  • 1. Department of Earth and Planetary Science,The University of Tokyo,7-3-1 Hongo,Bunkyo-ku,Tokyo 113-0033,Japan
  • 2. Graduate School of Science,Tohoku University,6-3,Aramaki-aza-aoba,Aoba-ku,Sendai,980-8578,Japan
  • 3. Geological Survey of Japan,National Institute of Advanced Industrial Science and Technology(AIST),Tsukuba Central 7,1-1-1 Higashi,Tsukuba,Ibaraki 305-8567,Japan
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摘要

关键词

Tides/Ocean bottom pressure/Slow earthquake/Seismicity/Kuroshio current

Key words

Tides/Ocean bottom pressure/Slow earthquake/Seismicity/Kuroshio current

引用本文复制引用

Yoshiyuki Tanaka,Hiromu Sakaue,Masayuki Kano,Suguru Yabe..A combination of tides and nontidal variations in ocean bottom pressure may generate interannual slip fluctuations in the transition zone along a subduction plate interface[J].大地测量与地球动力学(英文版),2023,14(1):43-51,9.

基金项目

We are grateful to the two anonymous reviewers and the editor who gave us valuable comments to improve the manuscript.We acknowledge the JMA for providing the earthquake catalog,the tide gauge record and the ocean model.We also acknowledge the Geospatial Information Authority of Japan for providing the GNSS data.For this study,we used the computer systems of the Earth-quake and Volcano Information Center of the Earthquake Research Institute,The University of Tokyo.This research was partly sup-ported by JSPS KAKENHI Grant Numbers JP16H02219,JP21H01187,JP21H05204,JP21K14022 and JP21H05203 and JST Grant Number JPMJMI18A1.Some figures were created using the Generic Mapping Tools[37]. ()

大地测量与地球动力学(英文版)

OACSCDEI

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