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首页> 外文期刊>Marine Geology >Nd, Sr isotopes and elemental geochemistry of surface sediments from the South China Sea: Implications for Provenance Tracing
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Nd, Sr isotopes and elemental geochemistry of surface sediments from the South China Sea: Implications for Provenance Tracing

机译:Nd,Sr同位素和南海表层沉积物的元素地球化学:物源追踪的意义

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摘要

The mineralogy, major and trace elements, and neodymium and strontium isotopes of surface sediments in the South China Sea (SCS) are documented with the aim of investigating their applicability in provenance tracing. The results indicate that mineralogical compositions alone do not clearly identify the sources for the bulk sediments in the SCS. The Nd isotopic compositions of the SCS sediments show a clear zonal distribution. The most negative ?_(Nd) values were obtained for sediments from offshore South China ( - 13.0 to -10.7), while those from offshore Indochina are slightly more positive (- 10.7 to - 9.4). The Nd isotopic compositions of the sediments from offshore Borneo are even higher, with ?_(Nd) ranging from - 8.8 to - 7.0, and the sediments offshore from the southern Philippine Arc have the most positive ?_(Nd) values, from - 3.7 to + 5.3.
机译:记录了南中国海(SCS)表层沉积物中的矿物学,主要元素和微量元素以及钕和锶同位素,旨在研究其在物源追踪中的适用性。结果表明,仅矿物成分并不能清楚地识别南海大块沉积物的来源。南海沉积物中的Nd同位素组成显示出明显的纬向分布。来自中国南方近海的沉积物获得最大负值Δ_(Nd)(-13.0至-10.7),而来自印度支那近海的沉积物Δ_(Nd)值则略为正值(-10.7至-9.4)。来自婆罗洲近海的沉积物的Nd同位素组成甚至更高,?_(Nd)的范围为-8.8至-7.0,而菲律宾南部弧形近海的沉积物的?_(Nd)值最大,为- 3.7至+ 5.3。

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