Multiple records from osmium, neodymium, and strontium isotope systems of the Nikubuchi ultramafic complex in the Sambagawa metamorphic belt, central Shikoku, Japan

• SENDA RYOKO

  Center for Chronological Research, Nagoya University

• KACHI TAKUYA

  Department of Earth and Planetary Sciences, Graduate School of Science, Nagoya University

• TANAKA TSUYOSHI

  Department of Earth and Environmental Sciences, Graduate School of Environmental Studies, Nagoya University

抄録

The isotopic compositions of Os, Nd, and Sr, as well as major elements of dunites, spinel lherzolites, websterite, and serpentinite from the Nikubuchi ultramafic cumulous complex in the Sambagawa metamorphic belt (SMB) were investigated. The Nikubuchi ultramafic complex is a layered cumulate and is surrounded by a metagabbro massif in the SMB. We obtained a Sm-Nd whole-rock isochron of the Nikubuchi complex with an age of 138 ± 18 (2σ) Ma and an initial ¹⁴³Nd/¹⁴⁴Nd ratio of 0.51270 ± 3. The Nikubuchi complex contains well preserved protogranular textures and cumulous layering structures, and has good correlation coefficients among the major element abundances, which indicate an event before the Sambagawa metamorphism. The ε_Nd values of 138 Ma (+3.5 to +5.3) correspond to the isotope signatures of ocean island basalt (OIB) or island arc basalt (IAB), and not mid-ocean ridge basalt (MORB). Taking the results of previous studies into consideration, the most likely origin of the Nikubuchi complex is that of a fragmented block of residual cumulate formed by the OIB magma chamber. The Rb-Sr isotope system has been disturbed by hydration and/or metamorphism after 138 Ma, and the Re-Os isotope system also has no valid isochron. One of the possible causes is that rhenium addition by hydration has occurred subsequent to 60 Ma. The results of the isotope systems show that hydration can cause disturbance in Re-Os systems but not in Sm-Nd systems. This probably reflects differences between these systems in resistance of the host phase.

収録刊行物

• ＧＥＯＣＨＥＭＩＣＡＬ　ＪＯＵＲＮＡＬ

  ＧＥＯＣＨＥＭＩＣＡＬ　ＪＯＵＲＮＡＬ 40 (2), 135-148, 2006

  一般社団法人日本地球化学会

キーワード

• ultramafic complex
• Re-Os isotope system
• Sm-Nd isotope system
• Sambagawa metamorphic belt
• cumulate complex

詳細情報

• CRID: 1390282679527870080
• NII論文ID: 10017551998
• NII書誌ID: AA00654975
• DOI: 10.2343/geochemj.40.135
• COI: 1:CAS:528:DC%2BD28Xks1Ojt7k%3D
• ISSN: 18805973
• ISSN: 00167002
• NDL書誌ID: 7854165
• Web Site: http://id.ndl.go.jp/bib/7854165
• Web Site: https://ndlsearch.ndl.go.jp/books/R000000004-I7854165
• Web Site: http://www.jstage.jst.go.jp/article/geochemj/40/2/40_2_135/_pdf
• 本文言語コード: en
• データソース種別:
  • JaLC
  • NDL
  • Crossref
  • CiNii Articles
• 抄録ライセンスフラグ: 使用不可