Detrital apatite fission track evidence for provenance change in the Subei Basin and implications for the tectonic uplift of the Danghe Nan Shan (NW China) since the mid-Miocene
作者: Xu LinDewen ZhengJimin SunBrian F. WindleyZhonghua TianZhijun GongYingying Jia
作者单位: 1Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
2State Key Laboratory of Earthquake Dynamics, Instituted of Geology, China Earthquake Administration, Beijing 100029, China
3CAS Center for Excellence in Tibetan Plateau Earth Sciences, China
4Department of Geology, The University of Leicester, Leicester LE1 7RH, UK
刊名: Journal of Asian Earth Sciences, 2015, Vol.111 , pp.302-311
来源数据库: Elsevier Journal
DOI: 10.1016/j.jseaes.2015.07.007
关键词: Detrital apatiteFission trackSubei BasinDanghe Nan ShanAltyn Tagh fault
英文摘要: Abstract(#br)The Subei Basin is located at the intersection of the northeastern end of the Altyn Tagh Fault (ATF) and the western end of the Danghe Nan Shan in the northeastern Tibetan Plateau. The Basin contains (up to) 4000m-thick Cenozoic terrestrial clastic sediments, which contain information on the uplift of the Danghe Nan Shan. In order to estimate the detrital apatite thermochronology with fission track dating, we collected eight sandstone samples from the Tiejianggou section of the Subei Basin, which has an established depositional age range from 22.8 to 9Ma. We found that a distinct change in slope of the peak age and lag time of the detrital apatite fission track occurred at ∼14Ma, which we interpret as a provenance...
全文获取路径: Elsevier  (合作)
影响因子:2.379 (2012)

  • Basin 水池
  • apatite 磷灰石
  • uplift 隆起
  • fission 分裂
  • tectonic 构造的
  • provenance 原产地
  • Miocene 中新世
  • track 径迹
  • since 以来
  • change 变化