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Geochemical characteristics and Genesis discussion with rock metailogenic belt of Geza island arc,Yunnan

机译:地球化学特征与Geza Island岩石岩石成群化带的成因探讨,云南

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Geza island arc located in the southwest Sanjiang tectonic igneous rock belts which was a products of Ganzi-Litang oceanic crust diving to Zhongdian Landmasses in late Triassic. Lithogeochemical characteristics shown that the porphyry(porphyrite) and island-arc granite rocks have the same rock series (high-K calc-alkaline) and the same genetic type (I-type granite); these rocks trace elements similar to the granite of island arc,which enriched in Ba, La, Hf, Au,chalcophile elements Cu,Pb, siderophile elements Mo, Ni, and depleted in Rb, Nb, P, Ti. In this region, the similarities of porphyry and local acidic volcanic rocks in the main elements, REE and other trace elements and the composition suggest that they both have the same or similar magmatic source rocks. It is shown that the characteristics of the rock with the island arc granite partial melting of source rock, that may come from the arc type volcano rock or island arc volcano rock cognate magma evolution.
机译:Geza Island Arc位于Sanjiang Sanjiang Tectonic Irgeous Rock Belts,这是甘孜兰塘海底潜水潜水的产品,潜水潜水。 石灰种化学特性表明,斑岩(卟啉)和岛弧花岗岩岩石具有相同的岩石系列(高k钙碱)和相同的遗传型(I型花岗岩); 这些岩石痕量的元素类似于岛弧的花岗岩,其富含Ba,La,Hf,Au,Chalcophile元素Cu,Pb,患者元素Mo,Ni和耗尽Rb,Nb,P,Ti。 在该地区,斑岩和局部酸性火山岩在主要元素,ree和其他微量元素和组合物中的相似性表明它们都具有相同或相似的岩石源岩。 结果表明,岩石与岛弧花岗岩部分熔化的岩石,可来自弧型火山岩或岛弧火山岩石同源岩浆进化。

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