Triple oxygen isotope constraints on the origin of ocean island basalts
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  • 英文篇名:Triple oxygen isotope constraints on the origin of ocean island basalts
  • 作者:Xiaobin ; Cao ; Huiming ; Bao ; Caihong ; Gao ; Yun ; Liu ; Fang ; Huang ; Yongbo ; Peng ; Yining ; Zhang
  • 英文作者:Xiaobin Cao;Huiming Bao;Caihong Gao;Yun Liu;Fang Huang;Yongbo Peng;Yining Zhang;Department of Geology and Geophysics, Louisiana State University;State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences;CAS Key Laboratory of Crust-Mantle Materials and Environments, School of Earth and Space Sciences,USTC;
  • 英文关键词:Triple oxygen isotope;;Helium isotope;;Ocean island basalts;;Mantle plume;;Mantle heterogeneity;;Crustal recycling
  • 中文刊名:DQHB
  • 英文刊名:地球化学学报(英文版)
  • 机构:Department of Geology and Geophysics, Louisiana State University;State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences;CAS Key Laboratory of Crust-Mantle Materials and Environments, School of Earth and Space Sciences,USTC;
  • 出版日期:2019-05-17
  • 出版单位:Acta Geochimica
  • 年:2019
  • 期:v.38
  • 基金:funding supports from the strategic priority research program (B) of Chinese Academy ofSciences (XDB18010104) and (XDB18010100);; Chinese NSF Project (41490635)
  • 语种:英文;
  • 页:DQHB201903001
  • 页数:8
  • CN:03
  • ISSN:52-1161/P
  • 分类号:3-10
摘要
Understanding the origin of ocean island basalts(OIB) has important bearings on Earth's deep mantle.Although it is widely accepted that subducted oceanic crust, as a consequence of plate tectonics, contributes material to OIB's formation, its exact fraction in OIB's mantle source remains ambiguous largely due to uncertainties associated with existing geochemical proxies. Here we show, through theoretical calculation, that unlike many known proxies, triple oxygen isotope compositions(i.e.D~(17 )O) in olivine samples are not affected by crystallization and partial melting. This unique feature, therefore, allows olivine D~(17 )O values to identify subducted oceanic crusts in OIB's mantle source. Furthermore, the fractions of subducted ocean sediments and hydrothermally altered oceanic crust in OIB's mantle source can be quantified using their characteristic D~(17 )O values. Based on published D~(17 )O data, we estimated the fraction of subducted oceanic crust to be as high as 22.3% in certain OIB, but the affected region in the respective mantle plume is likely to be limited.
        Understanding the origin of ocean island basalts(OIB) has important bearings on Earth's deep mantle.Although it is widely accepted that subducted oceanic crust, as a consequence of plate tectonics, contributes material to OIB's formation, its exact fraction in OIB's mantle source remains ambiguous largely due to uncertainties associated with existing geochemical proxies. Here we show, through theoretical calculation, that unlike many known proxies, triple oxygen isotope compositions(i.e.D~(17 )O) in olivine samples are not affected by crystallization and partial melting. This unique feature, therefore, allows olivine D~(17 )O values to identify subducted oceanic crusts in OIB's mantle source. Furthermore, the fractions of subducted ocean sediments and hydrothermally altered oceanic crust in OIB's mantle source can be quantified using their characteristic D~(17 )O values. Based on published D~(17 )O data, we estimated the fraction of subducted oceanic crust to be as high as 22.3% in certain OIB, but the affected region in the respective mantle plume is likely to be limited.
引文
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