首页> 外文期刊>Journal of the Geological Society of India >Geochemistry and petrogenesis of acid volcano-plutonic rocks of the Siner area, Siwana Ring Complex, Northwestern Peninsular India
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Geochemistry and petrogenesis of acid volcano-plutonic rocks of the Siner area, Siwana Ring Complex, Northwestern Peninsular India

机译:印度西北半岛西瓦纳环杂岩区锡纳地区酸性火山-古生岩的地球化学和岩石成因

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摘要

Petrochemical studies on acid plutonic (granite, microgranite) and volcanic (rhyolite, trachyte) rocks occurring in the Siner area of the Siwana Ring Complex, Malani Igneous Suite have been carried out. These rocks are characterized by high concentrations of SiO2, Na2O, K2O, Zr, Nb, Y and REE (except Eu) but low in MgO, Fe2O3(t), CaO, Cr, Ni, Sr; indicating their A-type affinity. Field studies in conjunction with the geochemical characteristic indicate that the magmatism in the Siner area is generally represented by peralkaline suite of rocks which are formed due to rift tectonics. It is also suggested that these acidic rocks could have been derived by low degree partial melting of crustal material. Characteristics of certain pathfinder elements such as Rb, Ba, Sr, K, Zr, Nb, REE and the ratios of K/Rb, Zr/Rb, Ba/Rb along with the multi elemental primitive mantle normalized spidergrams suggest that the Siner peralkaline granites and microgranites have the potential for rare metal and rare earth mineralizations.
机译:已经对发生在马拉尼火成岩组西瓦纳环网的锡纳地区的酸性多相岩(花岗岩,微花岗岩)和火山岩(流纹岩,菱形岩)进行了石油化学研究。这些岩石的特征是高浓度的SiO2,Na2O,K2O,Zr,Nb,Y和REE(Eu除外),而MgO,Fe2O3(t),CaO,Cr,Ni,Sr的含量低。表示它们的A型亲和力。结合地球化学特征的野外研究表明,西纳尔地区的岩浆作用通常由高碱性岩石组代表,这是由于裂谷构造而形成的。也有人认为这些酸性岩石可能是由于地壳物质的低度部分熔融而产生的。 Rb,Ba,Sr,K,Zr,Nb,REE等某些探路元素的特性以及K / Rb,Zr / Rb,Ba / Rb的比率以及多元素原始地幔归一化蜘蛛图表明Siner高碱性花岗岩微花岗岩具有稀土金属和稀土矿化的潜力。

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