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Isotope geochemistry of basaltic glasses from the Vance Seamounts, a near-ridge seamount chain adjacent to the Juan de Fuca Ridge.

机译:来自万斯海山的玄武岩玻璃的同位素地球化学,万斯海山是与胡安·德富卡山脊相邻的近岭海山链。

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摘要

Volcanic glass from 24 grab-samples from the Vance Seamounts, a chain of seven near-ridge seamounts (NRS) located adjacent to the southern Juan de Fuca Ridge (SJdF), was analysed for Sr, Nd, and Pb isotopic composition. The selected samples show a relatively large range of isotopic compositions (87Sr/86Sr from 0.702473 to 0.702755, 143Nd/144Nd from 0.513048 to 0.513182, and 206Pb/204Pb from 18.12 to 18.82).;The isotopic diversity, seen both within and among seamounts of the chain, is consistent with melt-induced mixing of a heterogeneous mantle source comprised of a depleted mantle (DM) matrix with 'plums' of HIMU(high micro)-like material. The observed isotopic compositions fall outside of previously observed compositional ranges from SJdF and neighbouring NRS lavas, but are consistent with compositions previously observed in lavas from the greater northeast Pacific. The data also support previous, recent melting events of the seamount source components beneath the adjacent SJdF.
机译:分析了来自范斯海山(Vance Seamounts)的24个采集样品中的火山玻璃,该链由七个与南胡安德富卡海岭(SJdF)相邻的近海岭海山(NRS)组成,分析了Sr,Nd和Pb同位素组成。选定的样品显示出较大范围的同位素组成(从0.702473至0.702755的87Sr / 86Sr,从0.513048至0.513182的143Nd / 144Nd和从18.12至18.82的206Pb / 204Pb)。这条链与由贫化地幔(DM)基质组成的异质地幔源与“李子”类HIMU(高微)材料的熔融诱导混合相一致。观测到的同位素组成不在先前观测到的SJdF和邻近NRS熔岩的组成范围之内,但与先前在大东北太平洋的熔岩中观测到的组成一致。数据还支持相邻SJdF下海山源组件的先前,最近的融化事件。

著录项

  • 作者

    Cornejo, Elizabeth Anne.;

  • 作者单位

    Carleton University (Canada).;

  • 授予单位 Carleton University (Canada).;
  • 学科 Geology.;Physical Oceanography.;Geochemistry.
  • 学位 M.Sc.
  • 年度 2008
  • 页码 181 p.
  • 总页数 181
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地质学;地质学;海洋物理学;
  • 关键词

  • 入库时间 2022-08-17 11:38:40

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