| 一种新的构造变形热年代学研究方法——显微构造变形热年代学 |
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| 引用本文： | 陈新跃,王岳军,范蔚茗. 一种新的构造变形热年代学研究方法——显微构造变形热年代学[J]. 华东地质学院学报, 2006, 29(3): 234-238 |
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| 作者姓名： | 陈新跃 王岳军 范蔚茗 |
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| 作者单位： | 湖南科技大学土木工程学院，中国科学院广州地球化学研究所，中国科学院广州地球化学研究所 湖南湘潭411201，中国科学院广州地球化学研究所，广东广州510640，广东广州510640，广东广州510640 |
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| 摘 要： | 显微构造变形热年代学是一种新兴的研究构造变形热年代学方法,能够解决一些常用方法无法解决的或很困难的构造问题。显微构造变形热年代学利用因构造变形事件而产生的新生矿物结晶年龄来测定小至一般的构造变形,大至区域构造乃至造山带或碰撞带构造变形的年龄,建立构造演化时间序列,并可以计算其变形速率或隆升速率。
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| 关 键 词： | 显微构造变形热年代学 矿物结晶年龄 构造变形年龄 |
| 文章编号： | 1000-2251(2006)03-234-05 |
| 收稿时间： | 2006-04-22 |
| 修稿时间： | 2006-04-22 |
A New Kind of Tectonic Deformation Thermochronology Research Method: Microstructure Deformation Thermochronology |
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| CHEN Xin-yue,WANG Yue-jun,FAN Wei-ming. A New Kind of Tectonic Deformation Thermochronology Research Method: Microstructure Deformation Thermochronology[J]. Journal of East China Institute of Technology, 2006, 29(3): 234-238 |
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| Authors: | CHEN Xin-yue WANG Yue-jun FAN Wei-ming |
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| Affiliation: | 1. School of Civil Engineering, Hunan University of Science and Technology, Xiangtan, HN 411201, China; 2. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, GD 510640 |
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| Abstract: | Microstructure deformation thermochronology is a new kind of tectonic deformation-termo-chronology research method,which interpreting some tectonic problems,which have been not interpretted or very difficult by common research methods.Microtectonic deformation-thermo-chronology can date tectonic deformation age precisely by dating new crystallizing minerals' crystallize age,which due to the tcetonic deformation event,range form small tectonic deformation to regional tectonic deformation,orogenic belt or collision zone tceonic deformation.Then,may built the order of tectonic evolution and assess the rates of deformation or accretion in the area. |
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| Keywords: | microstructure deformation thermochronology mineral crystallize age tectonic deformation age |
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