Journal of Jilin University(Earth Science Edition) ›› 2015, Vol. 45 ›› Issue (5): 1447-1459.doi: 10.13278/j.cnki.jjuese.201505116

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Early Cenozoic Altyn Mountains Uplift Recorded by Detrital Zircon Fission Track Age in Northwest Qaidam Basin

Wang Yadong1,2,3, Zheng Jianjing1,2, Sun Guoqiang1,2, Zheng Youwei1,2, Liu Xingwang1,2   

  1. 1. Lanzhou Center for Oil and Gas Resources, Institute of Geology and Geophysics, CAS/Gansu Provincial Key Laboratory of Petroleum Resources, Lanzhou 730000, China;
    2. Key Laboratory of Petroleum Resources Research, Chinese Academy of Sciences, Lanzhou 730000, China;
    3. School of Geographical and Earth Sciences, University of Glasgow, Glasgow G12 8QQ, UK
  • Received:2014-12-12 Published:2015-09-26

Abstract:

The Cenozoic uplift of Altyn Mountains has been closely concerned. A large number of thermochronology dates show that Altyn Mountains have periodically uplifted since Late Eocene (40-30 Ma). However, the thermochronology records of the early Cenozoic uplift of Altyn Mountains are rarely documented. The Cenozoic detrital zircon fission track age in the northwestern Qaidam basin shows that the detrital zircons came from the same source which did rapid uplift and exposed to the air in Early Cenozoic Paleocene-Middle Eocene(65-50 Ma), and provided the terrene clast. The previously reported analysis results suggested that the source of the western Qaidam basin were from Altyn Mountains. In consideration of the residual thickness of the sedimentary strata and sedimentary facies of Lulehe-Xiaganchaigou Formations in the western Qaidam basin, a brief and small-scale uplift of Altyn Mountains occurred in Early Cenozoic; which resulted in the small elevation difference between the mountains and the basin. Under the influence of the uplift, Qaidam terrain is high at southeast and low at northwest. The uplift represents the response of Altyn Mountains to the initial stage of collision between India and Eurasian plates. The zircon fission track thermal chronology data recorded the tectonic events of the middle-east part of Altyn Mountains in 65-50 Ma, which indicates the Cenozoic synchronicity uplifts of Tibetan plateau throughout south to north.

Key words: thermal chronology, zircon, Altyn Mountains, northwestern Qaidam basin, tectonic uplift, Early Cenozic

CLC Number: 

  • P588.212

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