Downloaded from http://sp.lyellcollection.org/ by guest on November 19, 2013 Geological Society, London, Special Publications Oligocene slow and Miocene−Quaternary rapid deformation and uplift of the Yumu Shan and North Qilian Shan: evidence from high-resolution magnetostratigraphy and tectonosedimentology Xiaomin Fang, Dongliang Liu, Chunhui Song, Shuang Dai and Qingquan Meng Geological Society, London, Special Publications 2013, v.373; p149-171. doi: 10.1144/SP373.5 Email alerting click here to receive free e-mail alerts when service new articles cite this article Permission click here to seek permission to re-use all or request part of this article Subscribe click here to subscribe to Geological Society, London, Special Publications or the Lyell Collection Notes © The Geological Society of London 2013 Downloaded from http://sp.lyellcollection.org/ by guest on November 19, 2013 Oligocene slow and Miocene–Quaternary rapid deformation and uplift of the Yumu Shan and North Qilian Shan: evidence from high-resolution magnetostratigraphy and tectonosedimentology XIAOMIN FANG1,2*, DONGLIANG LIU1,3, CHUNHUI SONG2, SHUANG DAI2 & QINGQUAN MENG2 1Key Laboratory of Continental Collision and Plateau Uplift & Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Shuangqing Road 18, Beijing 100085, China 2Key Laboratory of Western China’s Environmental Systems (Ministry of Education of China) and College of Resources and Environment, Lanzhou University, Gansu 730000, China 3Key Laboratory of Continental Dynamics of the Ministry of Land and Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China *Corresponding author (e-mail:
[email protected]) Abstract: Most existing tectonic models suggest Pliocene–Quaternary deformation and uplift of the NE Tibetan Plateau in response to the collision of India with Asia.