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Research on Trace Element Contents in Granitoids

Research Project

Project/Area Number 01540667
Research Category

Grant-in-Aid for General Scientific Research (C)

Allocation TypeSingle-year Grants
Research Field 鉱物学(含岩石・鉱床学)
Research InstitutionKumamoto University

Principal Investigator

TSUSUE Akio  Kumamoto Univ. Prof., 理学部, 教授 (20011512)

Co-Investigator(Kenkyū-buntansha) YOKOSE Hisayoshi  Kumamoto Univ. Res. Fellow, 理学部, 助手 (50230644)
MIZUTA Toshio  Akita Univ. Assoc. Prof., 鉱山学部, 助教授 (80094051)
Project Period (FY) 1989 – 1991
Project Status Completed (Fiscal Year 1991)
Budget Amount *help
¥1,600,000 (Direct Cost: ¥1,600,000)
Fiscal Year 1991: ¥300,000 (Direct Cost: ¥300,000)
Fiscal Year 1990: ¥300,000 (Direct Cost: ¥300,000)
Fiscal Year 1989: ¥1,000,000 (Direct Cost: ¥1,000,000)
KeywordsOuter Zone of Southwest Japan / I-type granitoids / S-type granitoids / Mineral assemblage / Butsuzo Tectonic Line / Middle Miocene / Omine district, Kii peninsula / Takatsukiyama / 花こう岩類 / REEパタ-ン / SrーRb図 / BaーRb図 / Eu異常 / ジュラ紀花こう岩類 / 飛騨変成帯 / 韓国 / 中新世花こう岩類 / 四国外帯 / 分別結晶作用
Research Abstract

The Outer Zone granitoids have been divided into two groups, namely, 1- and S-types. The granitoids occurring in the northern part of the Butsuzo Tectonic Line of the Outer Zone of Southwest Japan tend to have I-type characteristics, and S-type granitoids are generally restricted to the south. In addition to I- and S-type discrimination, some geochemical variations have been observed : K_2O, total Fe and normat6ive corundum increase toward the pacific side, while Fe_2O_3/FeO* (total Fe as FeO) ratio decreases. In this report we intend to report mineral assemblages of granitoids of the Omine district in the Kii peninsula and Takatsukiyama pluton in Shikoku. In the Omine district, granitoids are intermittently found along the trend of NS about 40 km long. The boundary of I- and S-type granitoids is located just about the Butsuzo Tectonic Line. The presence of amphibole is the characteristics of mineral assemblage of I-type granitoids, while the absence of amphibole and occasional presence of cordierite or garnet are the characteristics of S-type granitoids. The IS-type granitoids are found as separated plutons in the Omine district. The Takatsukiyarna pluton in Shikoku is located at 10 km south of the Butsuzo Tectonic Line. The pluton intruded into the Lower Shimanoto Supergroup of the Late Cretaceous age Depending on the field occurrence and mineral assembllage, the Takatsukiyama granitoids have been divided into three major petrographic types, namely, B-, W-C, W-A types. The B-type granitoid is found as a small ovoid body, 1 km X 0.5 km size, completely enclosed in the central part of the w-type body. The B- and W-A type granitoids belong to I-type, while the W-C type granitoids belong to S-type. The presence of the Land S-type granitoids within a single pluton is a characteristics of the pluton, and that must be the problem to solve.

Report

(3 results)
  • 1991 Annual Research Report   Final Research Report Summary
  • 1989 Annual Research Report
  • Research Products

    (20 results)

All Other

All Publications (20 results)

  • [Publications] Sato,K.,Sasaki,A.,Tsusue,A.and Nishimura,S.: "Th/U ratios of basement rocks and ore lead isotopes from the Korean peninsula:A reconnaissance(in Japanese)" Mining Geol.39. 219-222 (1989)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      1991 Final Research Report Summary
  • [Publications] Tsusue,A.,Mizuta,T.and Tamai,T.: "Mode of differentiation of granitic magmas in South Korea and Southwest Japan" Geochem.J.23. 271-278 (1989)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      1991 Final Research Report Summary
  • [Publications] Tsusue,A.,Dai,K.,Mizuta,T.and Tamai,T.: "A comparison of Jurassic granitoids between the Hida belt and South Korea" Minign Geol.40. 365-384 (1990)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      1991 Final Research Report Summary
  • [Publications] Tsusue,A.,Obata,M.,Furugori,S.,Dai,K.and Lee,I.H.: "Miocene granitoids of the Takatsukiyama pluton" Mining Geol.42. (1992)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      1991 Final Research Report Summary
  • [Publications] Tsusue,A.Dai,K.,Tanimoto,A.and Miyagawa,N.: "Miocene granitoids of the Ohmine district,Kii peninsula" Mining Geol.42. (1992)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      1991 Final Research Report Summary
  • [Publications] Sato, K., Sasaki, A., Tsusue, A. and Nishimura, S.: "Th/U ratios of basement rocks and ore lead isotope from Korean peninsula : A reconnaissance (in Japanese)" Mining Geol.39(3). 219-222 (1988)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      1991 Final Research Report Summary
  • [Publications] Tsusue, A., Mizuta, T. and Tamai, T.: "Mode of differentiation of granitic magmas in South Korea and Southwest Japan" Geochem. J.23(6). 271-278 (1989)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      1991 Final Research Report Summary
  • [Publications] Tsusue, A., Dai, K., Mizuta, T. and Tamai, T.: "A comparison of Jurassic granitoids between the Hida belt and South Korea" Mining Geol.40(6). 365-384 (1990)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      1991 Final Research Report Summary
  • [Publications] Tsusue, A., Obata, M., Furugori, S., Dai, K. and Lee, I. H.: "Miocene granitoids of the Takatsukiyama pluton" Mining Geol.42. (1992)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      1991 Final Research Report Summary
  • [Publications] Tsusue, A., Dai, K., Tanimoto, A. and Miyagawa, N.: "Miocene granitoids of the Omine district, Kii peninsula" Mining Geol.42. (1992)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      1991 Final Research Report Summary
  • [Publications] Sato,K.,Sasaki,A.,Tsusue,A.and Nishimura,S.: "Th/U ratios of basement rocks and ore lead isotopes from the Korean peninsula:A reconnaissance" Mining Geol.39. 219-222 (1989)

    • Related Report
      1991 Annual Research Report
  • [Publications] Tsusue,A.,Mizuta,T.and Tamai,T.: "Mode of differentiation of granitic magmas in South Korea and Southwest Japan" Geochem.J.23. 271-278 (1989)

    • Related Report
      1991 Annual Research Report
  • [Publications] Tsusue,A.,Dai,K.,Mizuta,T.and Tamai,T.: "A comparison of Jurassic granitoids between the Hide belt and South Korea" Mining Geol.40. 365-384 (1990)

    • Related Report
      1991 Annual Research Report
  • [Publications] Tsusue,A.,Obata,M.,Furugori,S.,Dai,K.and Lee,I.H.: "Miocene granitoids of the Takatsukiyama pluton" Mininig Geol.42. (1992)

    • Related Report
      1991 Annual Research Report
  • [Publications] Tsusue,A.,Dai,K.,Tanimoto,A.and miyagawa,N.: "Miocene granitoids of the Ohmine district,Kii peninsula" Mining Geol.42. (1992)

    • Related Report
      1991 Annual Research Report
  • [Publications] 佐藤和郎,佐々木昭,津末昭生,西村進: "コリア半島基盤岩のTh/U比と鉱床鉛同位体比:予察" 鉱山地質. 39. 219-222 (1989)

    • Related Report
      1989 Annual Research Report
  • [Publications] Tsusue,A.,Mizuta,T.and Tamai,T.: "Mode of differentiation of granitic magmas in South Korea and Southwest Japan." Geochemical Journal. 24. (1990)

    • Related Report
      1989 Annual Research Report
  • [Publications] Tsusue,A.,Dai,K.,Mizuta,T.and Tamai,T.: "A comparison of Jurassic granitoids between the Hida and South Korea." Mining Geoloogy. 40. (1990)

    • Related Report
      1989 Annual Research Report
  • [Publications] 古郡聡,津末昭生,小畑正明: "四国外帯の高月山花崗岩類について" 岩鉱. 85. (1990)

    • Related Report
      1989 Annual Research Report
  • [Publications] 代開秋,津末昭生: "飛騨変成帯の庄川花崗岩類について" 地質岩雑誌. 96. (1990)

    • Related Report
      1989 Annual Research Report

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Published: 1989-04-01   Modified: 2016-04-21  

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