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ZHANG Zhen-li, ZHANG Xin-quan, WEIWen-tong, PAN Zhi-long, LIU Ce, XU Yan-yan, TIAN Fen-ying, ZHAOWei-ying. A discussion on lithosphere evolution of Yanshan tectonic cycle in Hebei- Beijing-Tianjin region[J]. GEOLOGY IN CHINA, 2016, 43(3): 969-976. DOI: 10.12029/gc20160319
Citation: ZHANG Zhen-li, ZHANG Xin-quan, WEIWen-tong, PAN Zhi-long, LIU Ce, XU Yan-yan, TIAN Fen-ying, ZHAOWei-ying. A discussion on lithosphere evolution of Yanshan tectonic cycle in Hebei- Beijing-Tianjin region[J]. GEOLOGY IN CHINA, 2016, 43(3): 969-976. DOI: 10.12029/gc20160319

A discussion on lithosphere evolution of Yanshan tectonic cycle in Hebei- Beijing-Tianjin region

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Supported by China Geological Survey Program"the Regional Geology of the Beijing Municipality, Tianjin Municipality and Hebei Province"(No. 1212010911013).

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  • Received Date: September 05, 2015
  • Revised Date: January 24, 2016
  • Available Online: September 26, 2023
  • The lithospheric evolution of Hebei- Beijing- Tianjin region constitutes a complete tectonic evolution cycle. The lithosphere experienced multi- stage evolution, comprising tension cracking (non- orogenic) at the early stage of Late Triassic, stable transition at the late stage of Late Triassic (pre-orogenic), squeeze intraplate orogeny between the Early Jurassic and middle stage of Early Cretaceous (sym- orogenic), and stable transition during Cretaceous- Paleocene (post- orogenic). During the intraplate orogenic process of Yanshan tectonic cycle, the original cratonic lithosphere was strongly transformed and rebuilt, and formed a new orogenic lithosphere, which seems to have been the most important content of the Yanshan tectonic cycle and the substantive result of intraplate orogeny.
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