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粤北企岭岩体LA-ICP-MS锆石U-Pb年代学研究及成因分析

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通过采样分析粤北企岭花岗岩地球化学及LA-ICP-MS锆石U-Pb年龄,结果显示:岩石硅、铝含量较高,ω(SiO2)平均为73.41%,ω(Al2O3)平均为13.95%;钾大于钠,K2O/Na2O平均为1.89;相对富集强不相容元素为Rb、K、Th、U,明显亏损元素为Ba、Nb、Sr、Ti;ΣREE平均值209.19×10-6,Eu亏损明显,δEu平均为0.25;稀土元素表现为富集轻稀土向右倾的分配模式,LA-ICP-MS锆石年龄为154.3±3.1 Ma,反映是晚侏罗世岩浆活动的产物.综合分析认为,企岭岩体是在燕山早期南岭地区由于太平洋板块的俯冲导致先存的东西向薄弱断裂带重新被激活,在拉张伸展构造背景下,以古老地壳变质沉积岩为主的组分通过部分熔融的方式形成.
LA-ICP-MS Zircon U-Pb Chronology Research and Genetic Analysis of Qiling Granite in Northern Guangdong Province
The geochemistry and LA-ICP-MS zircon U-Pb age of Qiling granite in northern Guang-dong Province are analyzed by sampling.The results show that the content of Si and Al in the rocks is high,with an average of ω(SiO2)is 73.41%and ω(Al2O3)is 13.95%.The content of potassium is higher than that of sodium,and the average K2O/Na2O is 1.89.The highly enriched incompatible elements are Rb,K,Th and U,while the deficient elements are Ba,Nb,Sr and Ti.The average ΣREE is 209.19×10-6,the Eu defi-cit is obvious,and the average δEu is 0.25.The rare-earth elements are enriched in a right-leaning distribu-tion pattern,and LA-ICP-MS zircon is 154.3±3.1 Ma,reflecting the product of Late Jurassic magmatic ac-tivity.Comprehensive analysis shows that the Qiling pluton is reactivated by the subduction of the Pacific plate in the Nanling area in the early Yanshan period,and the components of the old crustal metamorphic sedimentary rocks are formed by partial melting under the background of tensile extension structure.

Qiling granitezircon U-Pb agegenetic analysis

丁建华、刘秋云、陈小祥

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广东省地质局第三地质大队

企岭岩体 锆石U-Pb年龄 成因分析

2024

现代矿业
中钢集团马鞍山矿山研究院有限公司

现代矿业

影响因子:0.33
ISSN:1674-6082
年,卷(期):2024.40(12)