Mesozoic–Cenozoic evolution and mechanism of tectonic geomorphology in the central North China Block: Constraint from apatite fission track thermochronology
作者: Xianzhi CaoSanzhong LiLiqing XuLingli GuoLiping LiuShujuan ZhaoXin LiuLiming Dai
作者单位: 1Key Lab of Submarine Geosciences and Prospecting Technique, Ministry of Education, Qingdao 266100, China
2Institute of Marine Geodynamics, College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
3ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS), The Institute for Geoscience Research (TIGeR), Department of Applied Geology, Curtin University, GPO Box U1987, Perth, WA 6845, Australia
刊名: Journal of Asian Earth Sciences, 2015, Vol.114 , pp.41-53
来源数据库: Elsevier Journal
DOI: 10.1016/j.jseaes.2015.03.041
关键词: North China BlockShallow-level structural patternDeep tectonicsTectonic geomorphologyApatite fission track
英文摘要: Abstract(#br)During the Mesozoic–Cenozoic, the central North China Block underwent complex tectonic transition and significant changes of tectonic geomorphology. This apatite fission track study shows that the west part of the Taihang Mountains experienced a rapid event which commenced before 160Ma and lasted until 135Ma, together with the extensive development of folds and thrusts, indicating this area experienced intense compression and uplift. Combined with the petrological and geological characteristics, the exhumation event represents the uplift of the Yanshanian North China Plateau and the Taihang Mountains inside it. During the Cenozoic, two episodes of rapid cooling events took place during 65–55Ma and after 25...
全文获取路径: Elsevier  (合作)
影响因子:2.379 (2012)

  • 磷灰石 构造的
  • track 径迹
  • Mesozoic 中生代
  • China 中国
  • fission 分裂
  • geomorphology 地貌学
  • tectonic 构造的
  • apatite 构造的
  • level 水准
  • pattern 模型
  • structural 构造