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滇西南澜沧江结合带中段云县花岗岩的地质特征及形成环境
引用本文:李宪坤,刘德利. 滇西南澜沧江结合带中段云县花岗岩的地质特征及形成环境[J]. 甘肃地质, 2008, 0(3): 80-88
作者姓名:李宪坤  刘德利
作者单位:甘肃省地矿局水文地质工程地质勘察院;中南大学地学与环境工程学院;
基金项目:中南大学地学环境工程学院与云南省云县矿业开发有限公司技术协作科研项目。
摘    要:南澜沧江结合带云县花岗岩体的岩石类型主要为黑云二长花岗岩,SiO2平均为68.57%,K2O/Na2O平均为1.67,相对富钾,岩石属高钾钙碱性系列。其岩石酸、碱度低于同类岩石平均值;而镁铁组分高于平均值,显示岩石偏中性,与同碰撞构造环境形成的花岗岩特征类似。Al2O3平均为13.66%,含量较高,ACNK平均为1.1,呈铝过饱和。CIPW计算结果,都出现标准矿物刚玉分子(〉1%)。岩石总体上相对富集大离子亲石元素,亏损高场强元素。稀土元素总量(EREE)高,平均240.75×10^-6。岩体轻稀土元素富集,重稀土亏损,(La/Yb)。为8.88-9.41,分异不是很大;Eu为中等负异常,δEu为0.52-0.57,经多种相关图解判别,岩石属S型花岗岩。其构造环境相当于大陆碰撞花岗岩类(CCG)。锆石颗粒U-Pb测年结果显示,源岩的形成年龄最晚是晋-7期(〉778Ma),岩体主体形成于华力西晚期一印支期。0206024-5k号锆石是岩浆成因锆石,该样品的206^Ph/238^U和207^Pb/235^U两个年龄(49Ma和61Ma)反映在云县岩体中可能存在喜山期岩浆活动。

关 键 词:云县  花岗岩  构造环境  锆石U-Pb年代

GEOLOGICAL CHARACTERISTICS AND TECTONIC SETTING OF THE YUNXIAN GRANITE IN THE MIDDLE PART OF SOUTH LANCANGJIANG CONVERGENT MARGIN, WESTERN YUNNAN PROVINCE
LI Xian-kun and LIU De-li. GEOLOGICAL CHARACTERISTICS AND TECTONIC SETTING OF THE YUNXIAN GRANITE IN THE MIDDLE PART OF SOUTH LANCANGJIANG CONVERGENT MARGIN, WESTERN YUNNAN PROVINCE[J]. Acta Geologica Gansu, 2008, 0(3): 80-88
Authors:LI Xian-kun and LIU De-li
Affiliation:1.Academy of Reconnaissance Hydrogeology and Engineering Geology;Gansu Province;Zhangye 734000;China;2.School of Geoscience and Environmental Engineering;Central South University;Changsha 410083;China
Abstract:Yunxian granite in the South Lancangjiang convergent margin is mainly diotite monzonite granite and belongs to potassium-rich calc-alkali series with SiO2=68.57 % and K2O/Na2O=1.67 on average. Both acidity and alkalinity of the rock are lower than the average and its mafic ingredient is higher than the average of homogeneous rocks which indicates that the rock tends to neutrality and is similar to syn-collision type granite. Yunxian granite is peraluminous with Al2O3=13.66% and ACNK=1.1 on average and corun...
Keywords:Yunxian  granites  tectonic settings  zircon U-Pb Age  
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