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Volcanostratigraphy and petrology of the Necgene volcanism in the morth kinki district

Research Project

Project/Area Number 60540527
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 InstitutionOsaka City University

Principal Investigator

FURUYAMA Katsuhiko  Faculty of Science, Osaka City University, assistant, 理学部, 助手 (10112525)

Project Period (FY) 1985 – 1987
Project Status Completed (Fiscal Year 1987)
Budget Amount *help
¥1,800,000 (Direct Cost: ¥1,800,000)
Fiscal Year 1987: ¥600,000 (Direct Cost: ¥600,000)
Fiscal Year 1986: ¥600,000 (Direct Cost: ¥600,000)
Fiscal Year 1985: ¥600,000 (Direct Cost: ¥600,000)
KeywordsMiocene / Pliocene / ソレアイト / 新第三紀 / 玄武岩 / 初生マグマ
Research Abstract

1. Neogene formation which is distributed in the north Kinki district is divided into two groups, the Miocene Hokutan and the Pliocene Teragi Groups. (1) The Hokutan Group is further divided into the Takayanagi, the Yoka, the Toyooka, the Muraoka.Amino and the Tango Formations in ascending order. (2) The Teragi Group is divided into the Basal Conglomerate, the Utaosa Rhyolite, the Yudani Conglomerate, the Haruki Mud and the Terada Volcanics.
2 (1) The lower part of the Yoka Formation is mainly composed of basic pyroclastic rocks and the upper part is mainly composed of basaltic lavas, which are olivine augite basalts in the Hamasaka and the Yoka districts, and olivine basalts in the Tango district. (2) The rhyolitic volcanic rocks are intercalated in the Toyooka Formation (Hide rhyolitea). The basaltic (Sugano Andesites) and rhyolitic lavas (Honzaka Rhyolites) are interbedded in the Amino formation. (3) The volcanic rocks in the Tango Formation (Nakahama Two pyroxene andesites) are charcterized by dacite. (4) The Teragi Group is characterized by the rhyolitic welded tuff in the lower part (Utaosa Rhyolite) and basaltic-andestic volcanic rocks in the upper part (Terada Volcanics).
3. (1) The volcanic rocks from the Yoka Formation range from the tholeiitic to the alkaline basalts. (2) The basalts from the Amino and the Teragi Formations are tholeiitic. (3) The andesites and dacites from the Amino and the Tango Formations are tholeiitic, and those from the Teragi Group are calc -alkaline. (4) The volcanism of the alkali basalits begun at the pleistocene age in the north Kinki district (Genbudo, Oginosen, Kannabe). (5) The basalts from the Yoka Formation are characterized by the low contents of HFSEs. On the contrary, those from the Teragi Group are rich in HFSEs. The fact suggests the difference of the mantle chemistry between the Miocene and the Pliocene ages in the north Kinki district.

Report

(2 results)
  • 1987 Final Research Report Summary
  • 1986 Annual Research Report
  • Research Products

    (5 results)

All Other

All Publications (5 results)

  • [Publications] 三宅康幸,古山勝彦: 日本地質学会関西支部報. 100. 27-29 (1986)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      1987 Final Research Report Summary
  • [Publications] 古山勝彦: 地学団体研究会第41回総会シンポジウム要旨集. 72-77 (1987)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      1987 Final Research Report Summary
  • [Publications] Miyake, Y. and Furuyama, K.: "The Tertiary tholeiites in Kinki district" Proceedings of Kamai Branch, Geological Society of Japan. No.100. 27-29 (1986)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      1987 Final Research Report Summary
  • [Publications] Furuyamam, K.: "Chemical compositional change of Neogene vokanic rocks in Sanin district" Abstmcts ; The 41st Annual Meeting of the Association for the Gedogical Collaboration in Japan. 72-77 (1987)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      1987 Final Research Report Summary
  • [Publications] 三宅康幸: 日本地質学会関西支部報. 100号. 27-29 (1986)

    • Related Report
      1986 Annual Research Report

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Published: 1987-03-31   Modified: 2016-04-21  

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