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1995 Fiscal Year Final Research Report Summary

DYNAMICS OF MAGMA GENERATION

Research Project

Project/Area Number 05231106
Research Category

Grant-in-Aid for Scientific Research on Priority Areas

Allocation TypeSingle-year Grants
Research InstitutionKYOTO UNIVERSITY

Principal Investigator

TATSUMI Yoshiyuki  KYOTO UNIVERSITY,FACULTY OF INTEGRATATED HUMAN STUDIES,PROFESSOR, 総合人間学部, 教授 (40171722)

Co-Investigator(Kenkyū-buntansha) FURUKAWA Yoshitsugu  KYOTO UNIVERSITY,FACULTY OF SCIENCES,ASSISTANT PROFESSOR, 理学部, 助手 (80222272)
SHIBUYA Hidetoshi  KUMAMOTO UNIVERSITY,FACULTY OF SCIENCES,ASSOCIATE PROFESSOR, 理学部, 助教授 (30170921)
SAKAI Satoshi  KYOTO UNIVERSITY,FACULTY OF INTEGRTATED HUMAN STUDIES,ASSOCIATE PROFESSOR, 総合人間学部, 助教授 (30144299)
HORI Tomotaka  KYOTO UNIVERSITY,GRADUATE SCHOOL OF HUMAN AND ENVIRONMENTAL STUDIES,PROFESSOR, 大学院・人間・環境学研究科, 教授 (40108981)
YANAGI Takeru  KYUSHU UNIVERSITY,FACULTY OF SCIENCES,PROFESSOR, 理学部, 教授 (90037234)
Project Period (FY) 1993 – 1995
KeywordsMAGMA / MANTLE DYNAMICS / SUBDUCTION ZONES / BACK ARC BASIN / HOTOSPOT
Research Abstract

The final goal of our magmalogical studies is comprehensive understanding of dynamic processes occurring in the Earth's mantle. Although the goal may be far beyond our present attainment, we have got some important results constraining such processes :
(1) Degrees of element transpor during dehydration of the subducted lithosphere have been documented based on highpressure experiments. The results can reasonable explain the geochemical characteristics of arc magmas.
(2) Seismic velociry of hydrous mantle materials has been obtained at high pressures and temperatures. The values are consistent with seismologically observed values, suggesting the location of hydrous peridotite layr at the base of the mantle wedge.
(3) Numerical simulation of mantle wedge temperature has demonstrated the location of high-temperature region within the mantle wedge, capbale for production of arc magmas.
(4) A comprehensive model for arc magma genesis, which can explain general characteristics of arc magmatism and is also constrained by the above results, has been proposed.
(5) Dynamic processes associated with back arc rifting, including geochemicale and thermal evolution of the mantle wedge, have been clarified.
(6) Geochemical works on S Pacific HIMU hotospot lavas have provided evidence for whole-mantle-scale recycling of oceanic crust materials.

  • Research Products

    (16 results)

All Other

All Publications (16 results)

  • [Publications] Y.Tatsumi: "Elastic wave velocities in isocnemical granvlite and amphibolre:origin of a low-velocity layer at the slab/mante wedge interface" Geophys.Res.Lett.21. 17-20 (1994)

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] Y.Tatsumi: "Thermal and geochemical evolution of the mantie weage in the NE Japan arc:I.Contri bution from experimental petrology" J.Geophys.Res.99. 22275-22283 (1994)

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] Y.Tatsumi: "Formation of a third volcahic chain in Kamchatka:gereration of unvsval aubduction-related magmas." Contrib.Mineral.Petrol.120. 117-128 (1995)

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] T.Kogiso: "HIMU ocean island basalts in southern Polynesia:new evidence for whole-mantle scale recycling of subdusted oceanlc crust" J.Geophys.Res.(in press). (1997)

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] Y.Tatsumi: "Subduction zone magmatism at clepths to 2900km:an overview" Bull.Volcanol.Soc.Japan. 42. 219-230 (1997)

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] Y.Tatsumi: "Trace element transport during dehydration pyocesses in the ocearic cyust:2,origin of chemical and physical characteristics in arc magmatism" Earth Planet,Sci.Lett.(in press). (1997)

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] Y.Tatsumi: "Blackwell" Subduction zone magmatism, 211 (1995)

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] 巽 好幸: "沈み込み帯のマグマ学-全マントルダイナミクスに向けて-" 東京大学出版会, 186 (1995)

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] Tatsumi, Y., Ito, K.and Goto, A.: "Elastic wave velocities in isochemical granulite and amphibolite : origin of a low-velocity layr at the slab/mantle wedge interface" Geophys.Res.Lett.21. 17-20 (1994)

    • Description
      「研究成果報告書概要(欧文)」より
  • [Publications] Tatsumi, Y., Furukawa, Y.and Yamashita, S.: "Thermal and geochemical evolution of the mantle wedge in the NE Japan arc : I.Contribution from experimental Petrology" J.Geophys.Res.99. 22275-22283 (1994)

    • Description
      「研究成果報告書概要(欧文)」より
  • [Publications] Tatsumi, Y., Kogiso, T.and Nohda, S.: "Formation of a third volcanic chain in Kamchatka : generation of unusual subduction-related magmas" Contrib.Mineral.Petrol.120. 117-128 (1995)

    • Description
      「研究成果報告書概要(欧文)」より
  • [Publications] Kogiso, T,Tatsumi, Y., Shimoda, H., and Barsczus, H.G.: "HIMU ocean island basalts in southern Polynesia : new evidence for whole-mantle scale recycling of subducted oceanic crust" J.Geophys.Res.(in press). (1997)

    • Description
      「研究成果報告書概要(欧文)」より
  • [Publications] Tatsumi, Y.and Kogiso, T.: "Trace element transport during dehydration processes in the subducted oceanic crust : 2, origin of chemical and physical characteristics in arc magmatism" Earth Planet.Sci.Lett.(in press). (1997)

    • Description
      「研究成果報告書概要(欧文)」より
  • [Publications] Tatsumi, Y., Arai, R., and Kogiso, T.: "Subduction zone magmatism at depths to 2900 km : an overview" Bull.Volcanol.Soc.Japan. 42. 219-230 (1997)

    • Description
      「研究成果報告書概要(欧文)」より
  • [Publications] Tatsumi, Y.and Eggins, S.: Subduction zone magmatism. Blackwell, Boston, 211 (1995)

    • Description
      「研究成果報告書概要(欧文)」より
  • [Publications] Tatsumi, Y.: Subduction zone magmatism : a contribution to whole mantle dynamics. University of Tokyo Press, 186 (1995)

    • Description
      「研究成果報告書概要(欧文)」より

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Published: 1999-03-09  

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