张八岭隆起中段池河地区瓦屋刘岩体地球化学特征与构造环境分析  

GEOCHEMICAL CHARACTERISTICS AND TECTONIC ENVIRONMENT ANALYSIS OF THE WAWULIU ROCK MASS IN THE CHIHE AREA IN THE MIDDLE PART OF THE ZHANGBALING UPLIFT

作　　者：钱辉[1] 王翔[1,2] 汪雅菲 邓佳良 QIAN Hui;WANG Xiang;WANG Ya-fei;DENG Jia-liang(Institute of Geological Survey of Anhui Province,Hefei,Anhui 230001,China;China University of Geosciences(Wuhan),Wuhan,Hubei 430074,China)

机构地区：[1]安徽省地质调查院,安徽合肥230001 [2]中国地质大学(武汉),湖北武汉430074

出　　处：《安徽地质》2020年第2期96-99,共4页Geology of Anhui

基　　金：安徽省国土资源厅公益性地质工作项目(2013-g-1)。

摘　　要：通过对张八岭隆起中段瓦屋刘岩体地球化学特征的研究,分析了岩浆源区特征与属性,为探讨该区构造-岩浆演化提供重要的信息。瓦屋刘岩体属高钾钙碱性岩系列,稀土元素、微量元素特征显示其为地壳深源物质部分熔融作用产物,并有源自交代地幔的热液流体参与。岩体地球化学特征与埃达克岩相近,形成于挤压、地壳加厚的构造背景。Based on study of geochemical characteristics of the Wawuliu rock mass in the middle part of the Zhangba Uplift,this paper analyzes the features and properties of the magmatic source area,providing important information for discussion of tectono-magmatic evolution in this area.The Wawuliu rock mass is of high-K calc-alkaline series.The characteristics of rare earth elements and trace elements show that the rock is the product of partial melting of deep-source materials in the crust,and is also involved in hydrothermal fluid sourced from the metasomatic mantle.The rock mass is geochemically similar to adakite that is formed in a tectonic setting of compression and crustal thickening.

关 键 词：二长花岗岩 花岗闪长岩 地球化学特征 瓦屋刘岩体 

分 类 号：P581[天文地球—岩石学]