新生代日本列島の火山活動とマントルダイナミクス

書誌事項

タイトル別名
  • Cenozoic Volcanisms and Mantle Dynamics in Japan
  • 新生代日本列島の火山活動とマントルダイナミクス--この10年における進展
  • シンセイダイ ニホン レットウ ノ カザン カツドウ ト マントルダイナミクス コノ 10ネン ニ オケル シンテン
  • ―この10年における進展―
  • Progress in the Last 10 Years

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説明

 The Japanese Islands have experienced subduction of the old Pacific Plate and the young Philippine Sea Plate, as well as back-arc basin opening, such as at the Kurile basin, Japan Sea, Shikoku basin, and Okinawa trough. This paper summarizes progress in understanding mantle dynamics beneath Japan in the past ∼10 years in terms of igneous petrology and geochemistry, seismology, and numerical simulation. The discussion is separated into four regions: Hokkaido, northeast and central Japan, southwest Japan (Chugoku and Shikoku districts), and Kyushu, from northeast to the southwest. Now that a massive amount of volcanic eruption age data and high-resolution seismic analyses have been accumulated for every region, we can discuss mantle dynamics within mantle wedge and back arc mantle in more detail than in the 20th century. Constraints related to water content, temperature, and melting process in the mantle from a natural sample are, however, still missing despite the importance of these factors when modeling mantle dynamics.

収録刊行物

  • 地学雑誌

    地学雑誌 119 (6), 1063-1078, 2010

    公益社団法人 東京地学協会

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