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Petrochemitry and zircon U-Pb age of Granodiorite-tonalite in the A'nyemaqen ophiolitic belt and its Tectonic significance

机译:阿尼玛琴蛇纹岩带花岗闪长岩-斑母岩的石化和锆石U-Pb年龄及其构造意义

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摘要

Zircon U-Pb age determination and petrochemistry research of the granodiorite-tonalite intruded in Buqinshn ophiolitic melange, the western sector of A'nyemaqen ophiolitic belt, are first done and Reported in this paper. Its zircon U-Pb age is 402±24Ma and belongs to Late Caledonian. The rock Belongs to calci-alkaline series, has the features of island-arc granite, which hints that oceanic crust Subduction and island-arc magmatism event occurred in the area in Early Paleozoic. The research Achievement is of great significance to re-understand the tectonic framework and evolution of the area, Even the Central Orogenic Belt.
机译:本文首先报道了在阿尼玛琴(A'nyemaqen)蛇纹岩带西部的Buqinshn蛇纹岩混杂岩中侵入的花岗闪长岩-斑母岩的锆石U-Pb年龄确定和岩石化学研究。锆石的U-Pb年龄为402±24Ma,属于晚古苏格兰。岩石属于钙-碱性系列,具有岛弧花岗岩特征,暗示古生代地区发生了洋壳俯冲和岛弧岩浆作用。研究成果对重新认识该地区甚至中央造山带的构造框架和演化具有重要意义。

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