• 责任者：Chen Xuanhua (Key Laboratory of Neotectonic Movement and Geohazard ; Ministry of Land and Resources ; Institute of Geomechanics ; Chinese Academy of Geological Sciences ; Beijing 100081 ; China) ; Michael W. ; Mcrivette
• 刊名：Geological Bulletin of China
• 出版年：2011
• 卷期：30(11)
• 关键词：隆起 ; uplifts ; 裂变径迹计时 ; fission-track dating ; 热年代学 ; thermochronology ; 昆仑山 ; Kunlun Mountains
• 页码：p.1647-1660
• 图表：7 illus., 1 table, 64 refs.
• 分类号：0300
• issnNo：ISSN1671-2552
• isbnNo：CN11-4648/P

Multiple phases of Mesozoic and Cenozoic cooling and uplifting events are derived from fission track (FT) dating of zircons and apatites and thermal history modeling of apatite FT ages from several plutons in East Kunlun near Golmud City. Two phases of Mesozoic cooling histories revealed by zircon FT ages are phase I in Jurassic (194.1～144.4 Ma)  and phase II in Early Cretaceous (115.7～100.2 Ma). According to the age comparability of the end of thrusting in Cenozoic phase II and the beginning of the major sinistral strike-slipping of Kunlun Fault, it is inferred that there was a deformational transfer from compressing to shearing at ～10.0 Ma.