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《Journal of Jilin University(Earth Science Edition)》 2011-05
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Zircon U-Pb Age and Tectonic Setting of Meta-Basalts of Liaohe Group in Helan Area,Liaoyang,Liaoning Province

WANG Hui-chu1,LU Song-nian1,CHU Hang1,XIANG Zhen-qun1,ZHANG Chang-jie2,LIU Huan1 1.Tianjin Center,China Geological Survey,Tianjin 300170,China 2.Shenyang Center,China Geological Survey,Shenyang 110034,China  
A lot of meta-basalts and mafic dykes occurred in the Northern Liaohe Group in Haicheng-Caohekou area,among which,the meta-basalts of Dashiqiao Formation in south Helan,Liaoyang,preserved a good pillow structure.The meta-pillow lava is chemically characterized by low alkaline,low K2O/Na2O ratios and iron-rich,which suggest that it belongs to island-arc tholeiite series.The REE and trace element characteristics indicate that the meta-pillow lava formed in the tectonic setting associated with the island-arc,likely back-arc basin rather than the continental rift.The study of isotopic chronology show that zircon SHRIMP U-Pb age of the meta-pillow lava is(1 869±28) Ma,of meta-diabase dyke is(1 828±13) Ma with a group of ~2 080 Ma captured zircon ages,and the zircon LA-ICP-MS U-Pb age of granite pegmatite is(1 869.7±7.6) Ma.Based on their occurrence,zircon dating and previous research data,it is suggested that the meta-pillow lava is formed at ~1880 Ma which could represent the forming age of Dashiqiao Formation,and the granite pegmatite is at ~1860 Ma which can be considered as a marker of the end of orogeny,and the meta-diabase dyke at ~1830 Ma which may indicates the beginning of post-orogeny extension.
【Fund】: 国家自然科学基金项目(40772120);; 国家地质矿产调查评价专项项目(1212010911005 1212011120154)
【CateGory Index】: P597.3
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