一の目潟と黒瀬のマントルカンラン岩捕獲岩のRb-Sr鉱物アイソクロン年代 Rb-Sr mineral isochron ages of mantle peridotite xenoliths from Ichinomegata and Kurose, Japan

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著者

    • 阿部 志保 ABE Shiho
    • 秋田大学工学資源学部応用地球科学教室 Institute of Applied Earthsciences, Faculty of Engineering and Resource Science, Akita University
    • 山元 正継 YAMAMOTO Masatsugu
    • 秋田大学工学資源学部応用地球科学教室 Institute of Applied Earthsciences, Faculty of Engineering and Resource Science, Akita University

抄録

Petrology, geochemistry and Rb-Sr chronology of seven spinel lherzolite-harzburgite xenolith samples from Ichinomegata, northeast Japan and Kurose, southwest Japan were studied. Whole rocks and the constituent minerals were analyzed for Rb and Sr contents and <sup>87</sup>Sr/<sup>86</sup>Sr ratios. The pure minerals were obtained by hand-picking and repetitive washing with hot acids (2M HCl, 5% HF) and distilled water.<br>     The peridotite xenoliths from Ichinomegata show wide variations in mineral and chemical compositions; clinopyroxene contents range from 4 to 13 volume%, Cr/(Cr+Al) ratios of spinel range from 0.19 to 0.41 and MgO contents of whole rock range from 38 to 46 weight%. The chondrite-normalized patterns of whole rock vary from LREE-depleted to flat or U-shaped. In spite of above petrographical and geochemical variations, <sup>87</sup>Sr/<sup>86</sup>Sr ratios of the clinopyroxenes are very uniform (0.7033∼0.7034). Rb-Sr mineral isochron ages of 208.9±80.1 Ma, 233.8±8.4 Ma, 252.9±19.8 Ma and 310.8±23.3 Ma are given by olivine, orthopyroxene, clinopyroxene and whole rock from each of four peridotite xenoliths. Since the peridotites have the relatively narrow range of ages and wide range of equilibrium temperatures, it is believed that a large-scale isotopic equilibration has occurred at various depths in the upper mantle beneath Ichinomegata.<br>     The peridotite xenoliths from Kurose show narrow ranges in mineral and chemical compositions; clinopyroxene contents range from 7 to 9 vol.%, Cr/(Cr+Al) ratios of spinel range from 0.28 to 0.31 and MgO contents of whole rock range from 41 to 43 wt.%. On the other hand, <sup>87</sup>Sr/<sup>86</sup>Sr ratios of the clinopyroxenes are very diverse (0.7034, 0.7039 and 0.7043), compared with those in Ichinomegata peridotites. The mineral isochrons based on the data of pyroxenes and whole rock also show very variable ages and initial <sup>87</sup>Sr/<sup>86</sup>Sr ratios. The Rb-Sr mineral isochron ages of 129.9±4.8 Ma, 312.8±16.7 Ma and 487.2±9.1 Ma indicate large intervals between the equilibration events.

収録刊行物

  • 岩鉱 : 岩石鉱物鉱床学会誌 : journal of mineralogy, petrology and economic geology  

    岩鉱 : 岩石鉱物鉱床学会誌 : journal of mineralogy, petrology and economic geology 94(8), 295-310, 1999-08 

    Japan Association of Mineralogical Sciences

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各種コード

  • NII論文ID(NAID)
    10002603603
  • NII書誌ID(NCID)
    AN10047992
  • 本文言語コード
    JPN
  • 資料種別
    ART
  • ISSN
    09149783
  • NDL 記事登録ID
    4853442
  • NDL 雑誌分類
    ZM46(科学技術--地球科学--岩石・鉱物・鉱床)
  • NDL 請求記号
    Z15-71
  • データ提供元
    CJP書誌  CJP引用  NDL  J-STAGE 
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