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首页> 外文期刊>International journal of chemistry and applications >Geochemistry of Shales of Barail group Occurring in and around Mandardisa, North Cachar Hills, Assam; India: Its Implications
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Geochemistry of Shales of Barail group Occurring in and around Mandardisa, North Cachar Hills, Assam; India: Its Implications

机译:阿萨姆邦北卡查尔山的曼达迪萨及其周围地区的Barail组页岩的地球化学;印度:其含义

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摘要

Geochemical studies of shale samples from Barail Group occurring in and around Mandardisa, North Cachar hills, Assam have been carried out The major, minor and trace elements present in the shale samples show significant results in determining provenance and source rock composition, tectonic setting, palaeoweathering, chemical maturity and palaeoclimate. The different bivariate plots suggest their derivation from felsic source rock of granitic dominated upper continental crust. In the CaO-K20-Na2O ternary plot of the shale samples fall in active continental margin. The CIA values indicate moderate to high degree of chemical weathering. The shales of the studied area show increasing chemical maturity under humid climatic condition.
机译:已对位于阿萨姆邦北部卡查尔山的曼达迪沙及其周围的Barail集团的页岩样品进行了地球化学研究。页岩样品中存在的主要,次要和微量元素显示出在确定物源和烃源岩组成,构造环境,古风化作用方面的重要结果,化学成熟度和古气候。不同的二元图表明它们源自花岗岩为主的上陆壳的长英质烃源岩。在CaO-K20-Na2O三元图的页岩样品落在活跃的大陆边缘。 CIA值指示中等至高度的化学风化。在潮湿的气候条件下,研究区域的页岩显示出越来越高的化学成熟度。

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