Acta Scientiarum Naturalium Universitatis Pekinensis ›› 2017, Vol. 53 ›› Issue (1): 57-65.DOI: 10.13209/j.0479-8023.2016.096

• Orginal Article • Previous Articles     Next Articles

Uplift-Exhumation History of Daqing Mountain, Inner Mongolia Since Late Mesozoic

Qinqin XU1,2,(), Jianqing JI2, Wentao ZHAO2, Xiangjiang YU2   

  1. 1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037
    2. The Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871
  • Received:2015-07-09 Revised:2016-04-15 Online:2016-11-17 Published:2017-01-20
  • Contact: Qinqin XU

内蒙古大青山晚中生代以来的隆升‒剥露过程

徐芹芹1,2,(), 季建清2, 赵文韬2, 于祥江2   

  1. 1. 中国地质科学院地质研究所, 北京 100037
    2. 造山带与地壳演化教育部重点实验室, 北京大学地球与空间科学学院, 北京 100871
  • 通讯作者: 徐芹芹
  • 基金资助:
    国家重点基础研究发展计划(2007CB411300)和中国地质调查局项目(12120115070301, 121201102000150009-01)资助

Abstract:

Four bedrock samples, collected from the eastern segment of Daqing Mountain, were analyzed using apatite fission-track (AFT) method. This elucidates the uplift-exhumation history of this area since the Late Cretaceous — in particular, when the present geomorphology of Daqing Mountain was shaped. The AFT ages range from 57.7±3.8 Ma to 50.4±3.3 Ma and the track length is between 10.7±0.4 μm and 9.9±0.1 μm. Modeling of the fission track data suggests two stages of rapid uplift and cooling, 100-90 Ma and since 13.5-7 Ma. The second cooling stage (since 13.5-7 Ma) was characterized by the fast uplift-exhumation in this area, resulting in the present geomorphology of Daqing Mountain.

Key words: apatite fission track, uplift-exhumation, Middle-Late Miocene, Daqing Mountain

摘要:

对大青山东段 4 件基岩样品进行磷灰石裂变径迹研究, 获得该区晚中生代以来的隆升-剥露历史, 并探讨大青山现代地貌的形成。样品的磷灰石裂变径迹年龄为 57.7±3.8~50.4±3.3 Ma, 封闭径迹长度分布在10.7±0.4~9.9±0.1 μm之间。热历史模拟结果表明, 大青山地区存在晚白垩世(约 100~90 Ma)和中-晚中新世(13.5~7 Ma)以来两个快速抬升冷却阶段, 13.5~7 Ma 以来是本区剥露最快的时期, 这一阶段的隆升造就现今大青山的地貌格局。

关键词: 磷灰石裂变径迹, 隆升-剥露, 中-晚中新世, 大青山

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