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首页> 外文期刊>Current Science: A Fortnightly Journal of Research >Geochemistry of sanukitoid series granitoids from the Neoarchaean Berach granitoid batholiths, Aravalli craton, northwestern Indian shield.
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Geochemistry of sanukitoid series granitoids from the Neoarchaean Berach granitoid batholiths, Aravalli craton, northwestern Indian shield.

机译:来自新印度西北贝拉奇花岗岩基岩,印度西北盾构Aravalli克拉通的sanukitoid系列花岗岩的地球化学。

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摘要

Geochemical studies of the Neoarchaean Berach granitoids, which are intrusive into the Banded Gneissic Complex of the Aravalli craton, have revealed the occurrence of granitoids of the sanukitoid series. They are calc-alkaline and enriched in both compatible and incompatible elements at a given SiO2 level. The granitoids are characterized by high K2O, high MgO, low Na2O/K2O, high Ba+Sr, negative Nb-anomaly and variable (Gd/Er)N. The geochemical characteristics of the Berach granitoids are strikingly similar to the Archaean sanukitoid series of rocks reported from else-where in the world. It is proposed that the Berach sanukitoid rocks were formed by partial melting of a metasomatized subcontinental lithospheric mantle, enriched in large ion lithophile elements.
机译:侵入到Aravalli克拉通带状片麻岩复合体中的新古柏Berach花岗岩的地球化学研究揭示了sanukitoid系列花岗岩的存在。它们是碱性钙,并在给定的SiO 2 含量下富含相容和不相容元素。花岗岩的特征是高K 2 O,高MgO,低Na 2 O / K 2 O,高Ba + Sr,负Nb -异常和变量(Gd / Er)N。 Berach花岗岩的地球化学特征与世界其他地方报道的太古岩系岩石相似。有人提出Berach sanukitoid岩石是通过变质交代的次大陆岩石圈地幔部分熔融而形成的,该地幔中富含大量的离子亲石元素。

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