Along‐arc variation in seismic velocity structure related to variable growth of arc crust in northern Izu‐Bonin intraoceanic arc

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  • Koichiro Obana
    Institute for Research on Earth Evolution Japan Agency for Marine‐Earth Science and Technology 3173‐25 Showa‐machi, Kanazawa‐ku, Yokohama 236‐0001 Japan
  • Shin'ichiro Kamiya
    Earthquake and Tsunami Research Project for Disaster Prevention Japan Agency for Marine‐Earth Science and Technology 3173‐25 Showa‐machi, Kanazawa‐ku, Yokohama 236‐0001 Japan
  • Shuichi Kodaira
    Institute for Research on Earth Evolution Japan Agency for Marine‐Earth Science and Technology 3173‐25 Showa‐machi, Kanazawa‐ku, Yokohama 236‐0001 Japan
  • Daisuke Suetsugu
    Institute for Research on Earth Evolution Japan Agency for Marine‐Earth Science and Technology 2‐15 Natsushima‐cho, Yokosuka 237‐0061 Japan
  • Narumi Takahashi
    Institute for Research on Earth Evolution Japan Agency for Marine‐Earth Science and Technology 3173‐25 Showa‐machi, Kanazawa‐ku, Yokohama 236‐0001 Japan
  • Tsutomu Takahashi
    Institute for Research on Earth Evolution Japan Agency for Marine‐Earth Science and Technology 3173‐25 Showa‐machi, Kanazawa‐ku, Yokohama 236‐0001 Japan
  • Yoshihiko Tamura
    Institute for Research on Earth Evolution Japan Agency for Marine‐Earth Science and Technology 2‐15 Natsushima‐cho, Yokosuka 237‐0061 Japan

書誌事項

公開日
2010-08
権利情報
  • http://onlinelibrary.wiley.com/termsAndConditions#vor
DOI
  • 10.1029/2010gc003146
公開者
American Geophysical Union (AGU)

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説明

<jats:p>The Izu‐Bonin arc is an intraoceanic island arc where the Pacific plate subducts beneath the Philippine Sea plate. Along‐arc variation in thickness of the arc crust has been observed by previous active seismic surveys beneath the Izu‐Bonin arc. We have imaged three‐dimensional (3‐D) seismic velocity structures in the northern Izu‐Bonin arc using arrival time data of the earthquakes during 80 days of observations by ocean bottom seismographs and three permanent island seismic stations. Our 3‐D velocity model indicates heterogeneous structure in the mantle wedge along the arc. Low‐velocity anomalies related to upwelling flow in the mantle wedge are not uniform beneath the volcanic front. Low‐velocity anomalies extending down to the subducting slab beneath the volcanic front coincide with thicker parts of the arc crust north of Aoga‐shima and south of Sumisu‐jima. This coincidence suggests that heterogeneous mantle upwelling flow fundamentally controls the growth of the arc crust. Along topographic highs in the forearc, low‐velocity anomalies in the crust and uppermost mantle coincide with positive magnetic anomalies suggesting the presence of a remnant arc, providing further evidence of this view of arc crust formation.</jats:p>

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