| 陕西紫阳辉长岩锆石U-Pb年龄及微量元素地球化学特征 |
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| 引用本文： | 谢巧勤,赵月领,张焕侠,陈天虎,徐晓春,薛怀民,赵建新.陕西紫阳辉长岩锆石U-Pb年龄及微量元素地球化学特征[J].地质科学,2014,0(2):456-471. |
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| 作者姓名： | 谢巧勤 赵月领 张焕侠 陈天虎 徐晓春 薛怀民 赵建新 |
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| 作者单位： | 1. 合肥工业大学资源与环境工程学院 合肥 230009;
2. Radiogenic Isotope Laboratory, Centre for Microscopy and Microanalysis, University of Queensland, Brisbane, Qld 4072, Australia;
3. 陕西省地质矿产勘查局物化探队 西安 710043;
4. 中国地质科学院地质研究所 北京 100037 |
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| 摘 要： | 陕西安康的瓦房店、紫阳、岚皋、镇坪和湖北竹溪一带的早古生代地层中广泛出露具双峰式岩浆岩组合的岩墙群。本文通过紫阳高滩辉长岩锆石LA-ICP-MS U-Pb年代学研究，获得其侵位年龄为410±4.5 Ma。高滩辉长岩具有类似OIB的稀土元素和微量元素分配特征，Th/Nb比值小于0.11，Nb/Zr大于0.15，显示其形成于与地幔柱活动相关的富集地幔源区。Nb/U、Ce/Pb比值及U、Th、Pb和Ni含量特征显示岩浆演化早期经历橄榄石和辉石的弱分离结晶作用，岩浆上升过程中几乎未受到地壳物质混染作用。高滩辉长岩年代学、微量元素地球化学特征及区域地质特征表明，早古生代晚期扬子陆块北缘地幔柱作用使得该区软流圈地幔上涌，导致扬子板块北缘陆内裂解，引发紫阳、岚皋一带早古生代晚期的基性岩浆作用。由于地幔深部热动力条件制约，这次大陆裂解事件未能持续。高滩辉长岩锆石年龄是对扬子板块北缘陆内裂解事件的响应。
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| 关 键 词： | 扬子板块北缘 辉长岩 锆石U-Pb定年 大陆裂解 |
| 收稿时间： | 2013-11-30 |
| 修稿时间： | 2013-11-30; |
Zircon U-Pb dating and trace elements geochemistry of the Gaotan gabbro from Ziyang County,Shaanxi Province |
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| Xie Qiaoqin,Zhao Yueling,Zhang Huanxia,Chen Tianhu,Xu Xiaochun,Xue Huaimin,Zhao Jianxin.Zircon U-Pb dating and trace elements geochemistry of the Gaotan gabbro from Ziyang County,Shaanxi Province[J].Chinese Journal of Geology,2014,0(2):456-471. |
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| Authors: | Xie Qiaoqin Zhao Yueling Zhang Huanxia Chen Tianhu Xu Xiaochun Xue Huaimin Zhao Jianxin |
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| Institution: | 1. School of Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009;
2. Radiogenic Isotope Laboratory, Centre for Microscopy and Microanalysis, University of Queensland, Brisbane, Qld 4072, Australia;
3. Geophysical and Geochemical Prospecting Team, Shaanxi Province Bureau of Geology and Mineral Resources Exploration and Exploitation, Xi'an 710043;
4. Institute of Geology, Chinese Academy of Geological Science, Beijing 100037 |
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| Abstract: | Basic dike swarms are widely distributed in the Ziyang-Langao-Zhenping area of Ankang in Shaanxi Province and Zhuxi area in Hubei Province,intruding the Early Paleozoic strata which characterized by bimodal volcanic association. The gabbro dikes emplacement dated 410±5 Ma by the LA-ICP-MS zircon U-Pb dating. They show the patterns of enriched LREE with high fractionation of light and heavy REE,and enrichment of incompatible elements in the primitive mantle-normalized spider-diagrams with peaks of Ba,Nb and Ti and valleys of Pb and U. The ratios of Th/Nb is less than 0.11 and those of Nb/Zr more than 0.15,indicating that they were derived from enriched mantle source closely related to the plume. The ratios of Nb/U, Ce/Pb and concentration of U,Th,Pb and Ni in the gabbro dikes indicate that the pyroxenes and olivines were main fractional minerals in the fractional crystallization during the magma evolution,and they were not affected by contamination of continental crust from the mantle to crust. These helps to infer that the extensional tectonics developed constrainedly in the Early Paleozoic by the mantle plume activities that happened at the boundary of paleocontinent on the northern margin of Yangtze Plate,thus producing the large group of basic dike swarms in these areas. The deep thermodynamic condition is responsible for the crustal extension and end. Thus the age of 410±4.5 Ma not only represents the magma emplacement,but also the extension evolution history of this continent crust rift from beginning to end in Silurian. |
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| Keywords: | Northtern margin of the Yangtze Plate Gabbro Zircon U-Pb LA-ICP-MS dating Continental rifting |
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