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Neodymium Isotope Ratios of Marine Barite: A Tool for Reconstruction of Paleocirculation

Neodymium Isotope Ratios of Marine Barite: A Tool for Reconstruction of Paleocirculation
海洋重晶石的钕同位素比:重建古循环的工具
批准号:
9521258
负责人:
Miriam Kastner
金额:
$8.96万
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
1996
资助国家:
美国
项目状态:
已结题
起止时间:
1996-01-15 至 1998-06-30

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项目成果

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中文摘要
翻译
9521258卡斯特纳·卡斯特纳将在海洋重晶石中开发ND同位素,以追踪水团的波动。这项技术应该有助于理解水团的发展及其在冰川-间冰期循环期间的运动。这项研究还应该有助于理解重晶石在水中形成的深度,这一问题已经困扰了一段时间。这一点很重要,因为沉积物中的重晶石已被用来指示地表水的生产力。***
英文摘要
9521258 Kastner Kastner will develop Nd isotopes in marine barite to trace fluctuations of water masses. This technique should be useful in understanding the development of water masses and their movement during glacial-interglacial cycles. This research should also lead to an understanding of what depth barite forms in the water, which has been a puzzle for some time. This is important because barite in sediments has been used to indicate the productivity of the surface waters. ***
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会议论文
Elemental and Isotopic Systematics in Erosional and Accretionary Subduction Zones, with Implications for Fluid Sources, Pathways, and Fluxes
Chlorine and Its Stable Isotope Budgets in Subduction Zones: Implications for Serpentinization and Cycling of Cl and Water
国内基金
海外基金
黄土蜗牛化石碳酸盐二元同位素("Clumped isotope")古温度重建研究
  • 批准号:
    41073065
  • 项目类别:
    面上项目
  • 资助金额:
    52.0万元
  • 批准年份:
    2010
  • 负责人:
    盛雪芬
  • 依托单位: