Understanding the uplift pattern in Mesozoic and Cenozoic, eastern   Dabie area, China using fission track dating of apatite

WU Qianhong  1  LIU Shunsheng  1  R.Jonckheere  2  G.A.Wagner  2  1

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Understanding the uplift pattern in Mesozoic and Cenozoic, eastern Dabie area, China using fission track dating of apatite

更新时间：2021-03-12

- Understanding the uplift pattern in Mesozoic and Cenozoic, eastern Dabie area, China using fission track dating of apatite
- NUCLEAR TECHNIQUES Issue 7, (2002)
- 作者机构：
  
  1. 中国科学院长沙大地构造研究所
  2. Max-Planck Institute für Kernphysik
  4. Heidelberg,D,6900
  5. ,Germany
- 作者简介：
- 基金信息：
  
  中国科学院院长基金特别支持项目;国家重点基础研究发展规划项目 (G19990 7550 4 )资助
- DOI：
  CLC： P597
- Published：01 July 2002
- 稿件说明：
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[1]吴堑虹,刘顺生,G.A.Wagner,R.Jonckheere.利用磷灰石裂变径迹定年方法探讨东大别山地区中、新生代构造抬升样式[J].核技术,2002(07):531-536.

WU Qianhong 1 LIU Shunsheng 1 R.Jonckheere 2 G.A.Wagner 2 1. Understanding the uplift pattern in Mesozoic and Cenozoic, eastern Dabie area, China using fission track dating of apatite[J]. Nuclear techniques, 2002, (7): 531-536.
[1]吴堑虹,刘顺生,G.A.Wagner,R.Jonckheere.利用磷灰石裂变径迹定年方法探讨东大别山地区中、新生代构造抬升样式[J].核技术,2002(07):531-536. DOI：

WU Qianhong 1 LIU Shunsheng 1 R.Jonckheere 2 G.A.Wagner 2 1. Understanding the uplift pattern in Mesozoic and Cenozoic, eastern Dabie area, China using fission track dating of apatite[J]. Nuclear techniques, 2002, (7): 531-536. DOI：

摘要

利用裂变径迹定年方法对东大别山地区进行了磷灰石裂变径迹年龄值和其空间分布样式及对中新生代构造活动示踪意义的初步探讨

并改进了传统的径迹统计方法。结果表明

研究区磷灰石裂变径迹年龄值为 5 9.4± 3.4— 10 5 .6± 9.8Ma

具有跨度较大以及由东向西趋向增大的特点 ;研究区自 95Ma以来其构造抬升是缓慢且不均匀 ;晓天 -磨子潭断裂中部在第三纪可能有逆冲 ;断裂活动应是该区构造抬升的主要控制因素

Abstract

By using the fission track dating technique

a preliminary study was carried out on the fission track ages (FTA) of apatite

their distribution patterns and hints over the tectonics activities during Mesozoic and Cenozoic in the east Dabie area. Attempts were also made to improve the conventional statistical method for the tracks. Ranging from 59.4±3.4Ma to 105.6±9.8Ma

the FTA results of apatite spread in a wide range and increased rapidly from the east to the west area. Sine 95Ma

the uplift rate has been quite slow and asymmetry. The FTA value in the middle area of Xiaotian-Mozitan Fault may imply its uplift in Cretaceous. The faulting should be the main control factor for the uplift of this area.

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