Late Mesozoic topographic evolution of western Transbaikalia:Evidence for rapid geodynamic changes f

• 作 者: A.V.Arzhannikova E.I.Demontero
• 机 构: InstituteoftheEarth’sCrust,LaboratoireG
  eosciencesRennes,GeologicalInstitute,A.P.VinogradovInstitute
• 出 处: 地学前缘:英文版
• 发表日期: 2020年5期
• 关键词: U–Pb detrital zircons dating Topographic evolution Mongol–Okhotsk collision TRAN
• 基金项目: supported by grants from the Russian Foundation for Basic Research(Grant No.17-05-00191),joint programme of Russian Foundation for Basic Research,Russia(No.13-05-91052),CNRS,France(PICS 4881)

The Mesozoic geodynamic evolution of Transbaikalia has been largely controlled by the scissors-like closure of the Mongol-Okhotsk Ocean that separated Siberia from Mongolia-North China continents.Following the oceanic closure,the tectonic evolution of tha