Detrital Zircon U⁃Pb Dating of Arkose⁃Quartzite in the Lugezhuang Formation in the Jingqishan Area, Jiaobei Terrane, and Its Geological Significance
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摘要: 荆山岩群是胶北地体最重要的古元古代变沉积岩系之一，经历了高角闪岩相‒麻粒岩相变质与韧性变形，准确限定其沉积时代与物质来源对探究胶‒辽‒吉带古元古代构造演化过程具有重要意义.本文利用LA-ICP-MS（激光剥蚀电感耦合等离子质谱仪）对旌旗山地区荆山岩群禄格庄岩组中长石石英岩进行了锆石U-Pb测年和稀土元素分析.根据碎屑锆石内部结构和年龄结果，认为在最年轻一组碎屑锆石中谐和的207Pb/206Pb加权平均年龄2 120 Ma，可以大致限定其原岩的最大沉积时代，两件样品获得的变质年龄分别为1 886±12 Ma与1 969±23 Ma，结合区内禄格庄岩组被2 103~2 085 Ma二长花岗质片麻岩侵入的地质关系，初步限定旌旗山地区禄格庄岩组的沉积时代约为2 100 Ma.长石石英岩中有效碎屑锆石年龄谱图呈现2 105 Ma主峰值年龄和2 185 Ma次峰值年龄，指示旌旗山地区禄格庄岩组的主要物源为古元古代（2 200~ 2 100 Ma）中‒酸性岩浆岩或再循环的产物，同时接受了少量太古宙的碎屑物质.综合胶‒辽‒吉带已发表的其他相关数据，认为以荆山岩群禄格庄岩组为代表的胶‒辽‒吉带南侧底部变沉积岩沉积时可能位于弧后盆地靠近岛弧一侧，以粉子山岩群小宋岩组为代表的胶‒辽‒吉带北侧底部变沉积岩则可能位于弧后盆地靠近太古宙大陆一侧.Abstract: The Jingshan Group, which has undergone high amphibolite to granulite facies metamorphism and ductile deformation, is one of the most widely distributed Paleoproterozoic meta-sedimentary rocks in the Jiaobei terrane of the Jiao-Liao-Ji Belt. Depositional timing and provenance of the Jingshan Group are vital for understanding the Paleoproterozoic tectonic evolution of the Jiao-Liao-Ji Belt. In this study, LA-ICP-MS (laser ablation inductively coupled plasma mass spectrometry) was used to analyze the zircon U-Pb ages and rare earth element compositions of arkose-quartzites in the Lugezhuang Formation of the Jingshan Group. Based on the internal structure of zircons and U-Pb ages, the concordant 207Pb/206Pb age of 2 120 Ma in the youngest group of detrital zircons is chosen as the maximal depositional timing of the Lugezhuang Formation. Two metamorphic ages in the two samples are 1 886±12 Ma and 1 969±23 Ma, respectively. Combined with the above data and the geological relationship which the Lugezhuang Formation was intruded by the 2 103-2 085 Ma granitic gneisses in the Jingqishan area, it is speculated that the depositional timing of the Lugezhuang Formation is circa 2 100 Ma. Detrital zircon age patterns from samples are characterized by the major peak of 2 105 Ma and secondary peak of 2 185 Ma. The new detrital age data reveals that the Lugezhuang Formation in Jingqishan area is mainly derived from Paleoproterozoic intermediate-acidic magmatic rocks or recycled products of the Paleoproterozoic (2 200-2 100 Ma) rocks with a small amount of Archaean detrital material. Combined with other published data of the Jiao-Liao-Ji Belt, it is speculated that the bottom meta-sedimentary rocks in the southern part of the Jiao-Liao-Ji Belt, which is represented by the Lugezhuang Formation of the Jingshan Group, may be deposited on the side of the continental arc of the back-arc basin, and the bottom metasedimentary rocks in the northern part of the Belt, which is represented by the Xiaosong Formation of the Fenzishan Group, may be close to the side of the Archean continent of the back-arc basin.
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Key words:
- Jingshan Group /
- Lugezhuang Formation /
- arkose-quartzite /
- zircon U-Pb dating /
- petrology
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图 1 华北克拉通古元古代造山/活动带(a)、东部陆块胶‒辽‒吉造山/活动带的地质简图(b)（修改自Zhao et al., 2012）
Fig. 1. Paleoproterozoic orogenic /mobile belts of the North China Craton (a), simplified geological map of the Paleoproterozoic Jiao-Liao-Ji orogenic /mobile belt in the Eastern Block, North China Craton (b) (modified after Zhao et al., 2012)
图 2 胶北地体前寒武纪变质地质简图（修改自刘平华等，2015）
Fig. 2. Simplified geological map of the Jiaobei Precambrian metamorphic basement (modified after Liu et al., 2015)
图 3 旌旗山地区地质简图(a)及荆山岩群地层划分与岩石单元(b)
Fig. 3. Simplified geological map of the Jingqishan area (a) and the stratigraphic subdivision and lithostratigraphic units of the Jingshan Group (b)
图 4 旌旗山地区荆山岩群禄格庄岩组长石石英岩野外露头照片
a，b，e. 禄格庄岩组长石石英岩远照；c，d，i. 禄格庄岩组长石石英岩风化露头近照；f. 长石石英岩中的花岗质细脉切层侵入；g. 长石石英岩中顺层侵入的石英脉；h. 禄格庄岩组变泥质岩中的小型褶皱正交偏光下可见因强烈的韧性剪切变形作用出现波状消光现象（图 5a~5d）
Fig. 4. Field photographs showing the outcrops of the arkose⁃quartzites from the Lugezhuang Formation of Jingshan Group from the Jingqishan area
图 5 荆山岩群禄格庄岩组长石石英岩代表性显微照片（a、c、e、g和i为单偏光，b、d、f和h为正交偏光）
Qz.石英；Pl.斜长石；Ser.绢云母；Mc.微斜长石
Fig. 5. Representative photomicrographs of the arkose-quartzites from the Lugezhuang Formation of the Jingshan Group (a, c, e, g, i are under plane-polarized light and b, d, f, h are under cross-polarized light)
图 6 荆山岩群禄格庄岩组长石石英岩(D0363-2, D5641-1)中代表性碎屑锆石CL图像及207Pb/206Pb年龄
Fig. 6. Cathodoluminescence images and 207Pb/206Pb ages of zircons of the arkose-quartzites (D0363-2, D5641-1) from the Lugezhuang Formation of Jingshan Group
图 7 旌旗山地区禄格庄岩组长石石英岩碎屑锆石谐和图（a, c, e）、碎屑锆石稀土元素配分模式图（b1, d, f）和碎屑锆石207Pb/206Pb年龄直方图（b2）（据Sun and McDonough, 1989）
Fig. 7. Concordia diagrams (a, c, e) REE patterns (b1, d, f) and histogram of 207Pb/206Pb age of detrital zircons (b2) from the Lugezhuang Formation in Jingqishan area (after Sun and McDonough, 1989)
图 8 胶‒辽‒吉带古元古代变沉积岩系碎屑锆石U-Pb年龄对比
数据来源：路孝平（2004）、Lu et al.（2006）、Luo et al.（2008）、秦亚等（2013）、孟恩等（2013）、谢士稳等（2014）、Lan et al.（2015）、Wang et al.（2017）、肖志斌等（2017）、Liu et al.（2018）、Zhang et al.（2018）、Xu et al.（2020）、张连祥等（2021a），以及本文数据）
Fig. 8. U-Pb age histogram of detrital zircons from the Paleoproterozoic metasedimentary rocks within the Jiao-Liao-Ji Belt
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