| 辽北西丰地区宝兴岩体LA-ICP-MS锆石U-Pb年龄及岩石地球化学特征 |
| |
| 引用本文： | 彭游博,宋淑娥,刘锦,张文静,王恩德,赵辰.辽北西丰地区宝兴岩体LA-ICP-MS锆石U-Pb年龄及岩石地球化学特征[J].地质通报,2017,36(10):1698-1707. |
| |
| 作者姓名： | 彭游博 宋淑娥 刘锦 张文静 王恩德 赵辰 |
| |
| 作者单位： | 1. 辽宁省地质矿产调查院, 辽宁 沈阳 110031;2. 东北大学资源与土木工程学院, 辽宁 沈阳 110004;3. 辽宁省地质实验研究所, 辽宁 沈阳 110032;4. 吉林大学地球科学学院, 吉林 长春 130000;5. 辽宁省地震局, 辽宁 沈阳 110034 |
| |
| 基金项目： | 中国地质调查局项目《辽东-吉南成矿带永吉—凤城地区地质矿产调查》（编号：DD20160049） |
| |
| 摘 要： | 宝兴岩体位于华北板块北缘陆缘活动带东段,岩性为花岗闪长岩,LA-ICP-MS锆石~(206)Pb/~(238)U年龄加权平均值为235.0±1.3Ma,属于中三叠世。岩石的K_2O/Na_2O平均值为1.07,属高钾钙碱性系列;富集大离子亲石元素,亏损高场强元素,具有活动陆缘钙碱性岩系特征;稀土元素总量平均值为147×10~(-6),稀土元素配分曲线右倾,属具中等负Eu异常的轻稀土元素富集、重稀土元素亏损型。通过岩石学、岩石地球化学及年代学研究,结合邻区构造演化研究,认为中三叠世研究区在伸展作用下岩石圈进行拆沉,从而形成大规模的岩浆活动。
|
| 关 键 词： | 中三叠世 LA-ICP-MS锆石U-Pb测年 宝兴岩体 花岗闪长岩 辽北地区 华北板块 |
| 收稿时间： | 2016/8/2 0:00:00 |
| 修稿时间： | 2017/3/19 0:00:00 |
LA-ICP-MS zircon U-Pb dating and geochemical characteris-tics of Baoxing rock mass in Xifeng area of northern Liaoning Province |
| |
| PENG Youbo,SONG Shu''e,LIU Jin,ZHANG Wenjing,WANG Ende and ZHAO Chen.LA-ICP-MS zircon U-Pb dating and geochemical characteris-tics of Baoxing rock mass in Xifeng area of northern Liaoning Province[J].Geologcal Bulletin OF China,2017,36(10):1698-1707. |
| |
| Authors: | PENG Youbo SONG Shu'e LIU Jin ZHANG Wenjing WANG Ende and ZHAO Chen |
| |
| Institution: | 1. Liaoning Survey Academy of Geology and Mineral Resources, Shenyang 110031, Liaoning, China;2. School of Resources and Civil Engineering/Northeast University, Shenyang 110004, Liaoning, China;3. Liaoning Geological Experiment Research Institute, Shenyang 110032, Liaoning, China;4. College of Earth Sciences, Jilin University, Changchun 130000, Jilin, China;5. Seismological Bureau of Liaoning Province, Shenyang 110034, Liaoning, China |
| |
| Abstract: | Located on the northern margin of North China Block, the Baoxing rock mass is mainly composed of granodiorite. Ac-cording to LA-ICP-MS zircon U-Pb dating, it was formed in Middle Triassic, with the 206Pb/238U age of 235.0±1.3Ma. The aver-age K2O/Na2O ratio is 1.07, indicating that the rocks belong to high-K calc-alkaline series. The rocks are enriched in LILE and de-pleted in HFSE, showing typical features of calc-alkaline series on an active continental margin. The average total amount of REE is 147×10-6, and the curve exhibits obvious right-inclined feature on REE distribution pattern, suggesting that the rocks are of the type of LREE enrichment and HREE depletion with medium negative Eu anomaly. According to the petrology, geochemistry and geo-chronology in combination with the tectonic evolution research on adjacent areas, lithospheric delamination occurred under the ex-tension in the study area, and then caused a large-scale magmatic activity in the Middle Triassic. |
| |
| Keywords: | Middle Triassic LA-ICP-MS zircon U-Pb dating Baoxing rock mass granodiorite northern Liaoning Province North China Block |
| 本文献已被 CNKI 等数据库收录！ |
| 点击此处可从《地质通报》浏览原始摘要信息 |
| 点击此处可从《地质通报》下载免费的PDF全文 |
|
