摘要
对东昆仑造山带五龙沟地区的猴头沟二长花岗岩开展了详细的岩相学、地球化学、锆石U-Pb年龄及Hf同位素的分析测试和研究工作。LA-ICP-MS锆石U-Pb测年表明,猴头沟二长花岗岩的206Pb/238U加权平均年龄值为（419.0±1.9）Ma,属于晚志留世。岩石地球化学数据表明：猴头沟二长花岗岩属于高钾钙碱性系列的A2型花岗岩,富SiO_2、K_2O、Y（〉33×10-6）和Yb,贫Al_2O_3和Sr（〈100×10^（-6））,具有强烈的负铕异常;Rb、Th、U、La、Ce、Nd相对富集,Nb、Ta、Ba、Sr、P、Ti亏损。锆石的Hf同位素研究表明,其εHf（t）值为0.2～5.1,对应二阶段模式年龄（TDM2）为1 066～1 371 Ma,由此推测花岗岩源区来自中元古代镁铁质下地壳部分熔融。微量元素及其特征比值的构造判别图解表明,猴头沟二长花岗岩形成于早古生代晚志留世东昆仑造山旋回的造山后伸展阶段。据此认为,原特提斯洋在东昆仑地区的最晚闭合时限应该不晚于晚志留世末期（～419 Ma）,而不是前人认为的早泥盆世。
This paper presents a detailed research work on LA-ICP-MS zircon U-Pb geochronology,geochemistry,and zircon Hf isotope of the Houtougou monzogranite in Wulonggou area of the easternKunlun orogen.The LA-ICP-MS zircon dating of the Houtougou monzogranite yields an average 206Pb/238 U age of（419.0±1.9）Ma,belonging to Late Silurian.Its geochemical features show that the Houtougou monzogranite belongs to a high-K calc-alkaline series of A2-type granite,and is characterized by high SiO_2,high K_2O,high Y（33×10^-6）and Yb,low Al_2O_3 and Sr（100×10^-6）,with a significant negative Eu anomaly,enriched in Rb,Th,U,La,Ce,and Nd,depleted of Nb,Ta,Ba,Sr,P,and Ti.The zircon Hf Isotopic data demonstrate that theirεHf（t）values range from 0.2to 5.1with the model ages（TDM2）of 1 066 to 1 371 Ma.It implies that their primary magma was likely derived from partial melting of lower Mesoproterozoic mafic crust.The trace elements and their characteristic ratios show that the Houtougou monzogranite emplaced in the post-orogenic stage of the eastern Kunlun orogen in Late Silurian.In view of the above facts,the closure of Proto-Tethys occurred in Late Silurian（~419 Ma）rather than Early Devonian in the eastern Kunlun orogen.
出处
《吉林大学学报（地球科学版）》
EI
CAS
CSCD
北大核心
2016年第2期443-460,共18页
Journal of Jilin University：Earth Science Edition
基金
中央高校基本科研业务费专项资金(JCKY-QKJC34)
国家自然科学基金项目(41572056)~~
关键词
猴头沟二长花岗岩
岩石地球化学
锆石U-PB定年
HF同位素
东昆仑
Houtougou monzogranite
lithological geochemistry
zircon U-Pb geochronology
zircon Hf isotopic systematic
eastern Kunlun orogen
