首页> 外文期刊>Current Science: A Fortnightly Journal of Research >Chemical and strontium isotopic composition of Kaveri, Palar and Ponnaiyar rivers: Significance to weathering of granulites and granitic gneisses of southern Peninsular India
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Chemical and strontium isotopic composition of Kaveri, Palar and Ponnaiyar rivers: Significance to weathering of granulites and granitic gneisses of southern Peninsular India

机译:Kaveri,Palar和Ponnaiyar河流的化学和锶同位素组成:对印度半岛南部南部的粒状花岗岩和花岗片麻岩的风化意义

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摘要

Strontium (Sr) isotope ratios and major ion abundance were determined on water samples of Kaveri, Palar and Ponnaiyar rivers, collected during the NE monsoon of 2005, when there was unusually heavy rainfall. Sr isotope ratios combined with major ion concentrations were used to determine relative contribution of Sr and major ions by weathering of various rock types exposed in the drainage basin. super(87)Sr/ super(86)Sr ratios were well correlated to Ca/Sr and Mg/Sr ratios in water samples indicating mixing of water with solute load essentially derived by weathering of granitoid gneisses, mafic volcanics and carbonates of the Archean schist belts in the upper reaches with the water draining felsic granulites in the lower reaches.
机译:测定了2005年东北季风期间Kaveri河,Palar河和Ponnaiyar河的水样品中锶(Sr)的同位素比率和主要离子丰度,当时降雨异常多。通过对流域暴露的各种岩石进行风化,使用Sr同位素比与主要离子浓度的组合来确定Sr和主要离子的相对贡献。 super(87)Sr / super(86)Sr比值与水样品中的Ca / Sr和Mg / Sr比值相关性很好,表明水与溶质负荷的混合主要是由于太古代片岩的花岗岩型片麻岩,镁铁质火山岩和碳酸盐的风化上游的河床带中,排水的长英质花岗石流在下游。

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