摘要
针对对铜陵桂花冲花岗闪长斑岩进行岩石学、岩石地球化学及锆石U-Pb同位素年代学研究,结果表明该花岗闪长斑岩高硅富碱(w(SiO2)平均为63.60%,w(Na2O+K2O)平均为7.09%,K2O/Na2O为0.51~0.68),属高钾钙碱性系列岩石。岩石稀土总量低(ΣREE在187.43×10-6和209.19×10-6之间),但轻稀土富集而重稀土亏损(ΣLREE/ΣHREE为15.00~16.49,(La/Yb)N为22.37~28.45),且具弱负Eu异常(δEu在0.75~0.83,平均为0.80)。同时,岩石富集大离子亲石元素(Rb,Ba,Th和U),而亏损高场强元素(Nb和Ta)。锆石LA-ICP-MS U-Pb定年测得花岗闪长斑岩年龄为(138.3±1.4)Ma,表明该岩体的形成时代为早白垩世,与铜陵矿集区中生代主要成矿岩体的年龄(137.5 Ma±1.1Ma^151.8Ma±2.6Ma)一致。该花岗闪长斑岩形成于碰撞后构造环境,是由壳幔混合岩浆冷却结晶形成的。
Petrologic and geochemical features and zircon U-Pb isotope age of the Guihuachong granodiorite porphyry in Tongling are studied.It shows that the rock is rich in w(SiO2)(averagely 63.60%)and alkali(averagely 7.09%),with smaller ratios of w(K2O/Na2O)(0.51-0.68),indicating that it belongs to high-K calc-alkaline series.It is characterized by low contents ofΣREE(187.43×10-6-209.19×10-6),high ratios ofΣLREE/ΣHREE(15.00-16.49)and(La/Yb)Nvalues(22.37-28.45),and a little negative Eu anomalies(δEu 0.75-0.83,averagely0.80).The rock is enriched in large iron lithophile elements(Rb,Ba,Th,and U)and depleted in high field strength elements(Nb and Ta).LA-ICP-MS zircon U-Pb age of the granodiorite porphyry is defined to be(138.3±1.4)Ma,suggesting that the rock was formed at the beginning of the Early Cretaceous Period,corresponding to the age(137.5Ma±1.1Ma-151.8Ma±2.6Ma)of main Mesozoic metallogenic plutons in Tongling.It is considered that this granodiorite porphyry was formed by cooling and crystallization of magma with mixing source of mantle and crust in the post-collision tectonic environment.
出处
《矿物岩石》
CAS
CSCD
北大核心
2015年第1期82-90,共9页
Mineralogy and Petrology
基金
中国地质调查局项目(12120113069900)
关键词
桂花冲花岗闪长斑岩
地球化学
锆石U-PB定年
安徽铜陵
Guihuachong granodiorite porphyry
geochemistry
zircon U-Pb dating
Tongling in Anhui Province