GEOCHRONOLOGY AND GEOCHEMISTRY OF THE LAMPROPHYRE DIKES IN QIXIA AREA, SHANDONG PROVINCE: Geological Implication
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摘要:
对山东栖霞河西夼地区的煌斑岩脉进行了岩相学、锆石U-Pb年代学和岩石地球化学研究. 锆石U-Pb测年结果显示, 煌斑岩中锆石年龄可以分为151~163 Ma、212~230 Ma、1 822~1 962 Ma及2 431~(2 613±37)Ma四个年龄区间. 其中8颗年轻锆石的206Pb/238U年龄介于(151±2)~(163±4)Ma之间, 加权平均年龄为153.7±2.8 Ma, 认为这一年龄代表了其形成时代. 其余锆石均为继承锆石, 指示在岩浆活动过程中受到了壳源物质的混染. 岩石地球化学的分析结果表明, 研究区煌斑岩具有Rb、Ba、Th、Pb及轻稀土元素富集, Ta、Nb、Zr、Hf、Ti等元素相对亏损的特征. 综合认为研究区煌斑岩形成于太平洋板块向欧亚板块俯冲背景下的火山弧环境, 在上升过程中受到了壳源物质的混染.
Abstract:The paper studies the petrography, zircon U-Pb chronology and petrogeochemistry of the lamprophyre dikes in Hexikuang area of Qixia, Shandong Province. The zircon U-Pb dating results show that the age of zircons in the lamprophyre can be divided into four age intervals: 151-163 Ma, 212-230 Ma, 1 822-1 962 Ma and 2 431-(2 613±37) Ma. The 206Pb/238U ages of eight young zircons range from (151±2) to (163±4) Ma, with the weighted mean age of 153.7±2.8 Ma, which represents its formation age. The others are inherited zircons, indicating that they are contaminated by crust-derived materials during magmatic activity. The lithogeochemical analysis results reveal that the lamprophyre in the area is characterized by enrichment of Rb, Ba, Th, Pb and LREEs, and relative depletion of Ta, Nb, Zr, Hf and Ti. From the above, it is concluded that the lamprophyre was formed in the volcanic arc environment under the background of subduction of Pacific Plate beneath Eurasian Plate, and was contaminated by crust-derived materials during its ascent.
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Key words:
- lamprophyre /
- zircon U-Pb geochronology /
- lithogeochemistry /
- petrogenesis /
- Shandong Province
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图 1 研究区地质图(据文献[17]修改)
Figure 1.
图 5 煌斑岩的TAS分类图和K/Al-K/(K+Na)图(据文献[23])
Figure 5.
图 6 煌斑岩球粒陨石标准化稀土元素配分图和原始地幔标准化微量元素蛛网图(球粒陨石和原始地幔标准化数据引自文献[26])
Figure 6.
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