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海南五指山地区花岗片麻岩锆石LA-ICP-MS U-Pb年代学特征及其地质意义
引用本文:陈新跃,王岳军,范蔚茗,张菲菲,彭头平,张玉芝.海南五指山地区花岗片麻岩锆石LA-ICP-MS U-Pb年代学特征及其地质意义[J].地球化学,2011(5):454-463.
作者姓名:陈新跃  王岳军  范蔚茗  张菲菲  彭头平  张玉芝
作者单位:[1]湖南科技大学地质研究所,湖南湘潭411201 [2]中国科学院广州地球化学研究所,广东州510640
基金项目:国家自然科学基金(40902062, 40825009, 40830319); 国家重点基础研究发展计划项目(2007CB411403); 高等学校特色专业建设点项目(TS11027)
摘    要:海南五指山地区出露大面积花岗片麻岩,且广泛发育NW向定向变形构造,表明经历了明显的动力变形变质作用;4个花岗片麻岩样品的LA-ICP-MS锆石U-Pb年代学测试数据表明它们形成于263~269 Ma,代表了中二叠世的一次重要地质构造热事件.结合前人研究成果认为,海南五指山地区263~269Ma花岗片麻岩可能形成于华南与...

关 键 词:花岗片麻岩  锆石  LA-ICP-MS  U-Pb年代学  五指山地区  海南岛

Zircon LA-ICP-MS U-Pb dating of granitic gneisses from Wuzhishan area, Hainan, and geological significances
CHEN Xin-yue,WANG Yue-jun,FAN Wei-ming,ZHANG Fei-fei,PENG Tou-ping,ZHANG Yu-zhi.Zircon LA-ICP-MS U-Pb dating of granitic gneisses from Wuzhishan area, Hainan, and geological significances[J].Geochimica,2011(5):454-463.
Authors:CHEN Xin-yue  WANG Yue-jun  FAN Wei-ming  ZHANG Fei-fei  PENG Tou-ping  ZHANG Yu-zhi
Institution:1. Institute of Geology, Hunan University of Science and Technology, Xiangtan 411201, China;2.Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China)
Abstract:Better understanding on the formation and evolution of the convergence of the South China with
Indochina Blocks had been restricted by the lack of precise geochronological data. Syntectonic granitic gneisses with NW-trending gneissic foliations are widely distributed in Wuzhishan area, Hainan Island. LA-ICP-MS zircon U-Pb dating of four samples yielded crystallization ages of 263–269 Ma, representing a key thermal-tectonic event in the Middle Permian. Combined with previous work, our dating results for the Wuzhishan orthogneiss suggest the Wuzihshan syntectonic granitic gneisses were derived from the convergence of the South China with Indochina Blocks. This age (263–269 Ma) might represent the initial time of the collision between the South China and Indochina Blocks.
Keywords:granitic gneisses  zircon  LA-ICP-MS  U-Pb dating  Wuzhishan area  Hainan Island
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