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Role of subducting component and sub-arc mantle in arc petrogenesis: Andaman volcanic arc

机译:俯冲分量和亚弧幔在弧成岩作用中的作用:安达曼火山弧

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摘要

Geochemical proxies, especially the trace element ratios of arc lavas from Barren and Narcondam Islands of the Andaman-Nicobar Islands group, display dissimilar characteristics. Narcondam lavas (mostly andesitic) are typically characterized by high Ba/La, Ba/Nb and Th/Nd ratios, reflective of the imprint of substantial subduction component in the form of sediment fluid and melt. On the other hand, Barren lavas (mostly basaltic) show relatively high Ba/Th ratios, indicative of fluid-induced subduction component, mainly signature-inducing fluid component, derived from altered ocean crust.
机译:地球化学代理,特别是安达曼-尼科巴群岛组的Barren和Narcondam群岛的弧熔岩的痕量元素比率显示出不同的特征。 Narcondam熔岩(主要是安山岩)通常以高Ba / La,Ba / Nb和Th / Nd比为特征,反映出以泥沙流体和熔体形式存在的大量俯冲成分的印记。另一方面,贫瘠的熔岩(大部分为玄武质)显示出相对较高的Ba / Th比值,表明流体诱导的俯冲成分,主要是特征性诱导的流体成分,源于改变的海洋地壳。

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