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    Volume 37 Issue S1
    Nov.  2021
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    Article Navigation >  Earth Science  > 2012  >  37(S1): 93-100
    LI Jiang-shan, FANG Nian-qiao, SHI Xue-fa, REN Xiang-wen, LIU Ji-hua, CUI Ying-chun, 2012. Helium and Argon Isotopic Compositions of Various Crustal Layers of a Co-Rich Fe-Mn Crust from Central Pacific. Earth Science, 37(S1): 93-100. doi: 10.3799/dqkx.2012.S1.009
    Citation: LI Jiang-shan, FANG Nian-qiao, SHI Xue-fa, REN Xiang-wen, LIU Ji-hua, CUI Ying-chun, 2012. Helium and Argon Isotopic Compositions of Various Crustal Layers of a Co-Rich Fe-Mn Crust from Central Pacific. Earth Science, 37(S1): 93-100. doi: 10.3799/dqkx.2012.S1.009
    shu

    Helium and Argon Isotopic Compositions of Various Crustal Layers of a Co-Rich Fe-Mn Crust from Central Pacific

    doi: 10.3799/dqkx.2012.S1.009
    • 1.

      Key Laboratory of Marine Sedimentology & Environmental Geology, the First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China

    • 2.

      Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China

    • 3.

      School of Marine, University of China Geosciences, Beijing 100083, China

    • Received Date: 2011-12-05
      Available Online: 2021-11-15
    • Publish Date: 2012-05-01
      Abstract
    • The noble gas isotopes abundance and composition were determined for various layers of a Co-rich Fe-Mn crust from seamount MH in the central Pacific. The He isotopic compositions of this Co-rich crust are similar to those of the abyssal sediments, and are mainly originated from the cosmic dust. 3He contents of the Co-rich crust are nearly constant throughout the section, but the 3He content increases significantly in 8 Ma, which is 4-5 times those of other samples, which responds to the 3He content maximum of the abyssal sediment in 8 Ma. In non-phosphatized Fe-Mn crust layers, the 3He/4He ratios of D4, D5 and D7 are also equivalent to the 3He/4He values n×102 Ra of the abyssal sediments. The 3He/4He ratios in phosphatized layers are relatively low, which resulted from incorporation of carbonate fluorapatite concentrates with enriched 4He, and depleted 3He during phosphatization. The loose layers of the Fe-Mn crust are relatively advantageous to adsorbing of Ar, and the majority of Ar in the crust possibly adsorbs directly from ambient sea water in the crust growth process.

       

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