A thermochronological perspective on the morphotectonic evolution of the southeastern Tibetan Plateau
Tian, Yuntao1; Kohn, Barry P.1; Gleadow, Andrew J. W.1; Hu, Shengbiao2
刊名JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2014
卷号119期号:1页码:676-698
关键词landscape evolution Tibetan Plateau thermochronology continental tectonics
ISSN号2169-9313
DOI10.1002/2013JB010429
文献子类Review
英文摘要A large part of the southeastern Tibetan Plateau (TP) is characterized by low-relief surfaces at high elevations (>3.5km). The origin of these landscapes and their geodynamic implications with regard to evolution of the southeastern TP has been the subject of considerable debate. Focusing on this topic, this study utilizes fission track and (U-Th)/He thermochronology to reconstruct the thermal history of the Late Triassic Daocheng granite, on which a low-relief high-elevation landscape has developed. Results suggest that the plateau surface experienced widespread Late Jurassic to Early Cretaceous cooling (at a rate of similar to 1-2 degrees C/Ma), followed by minimal regional cooling (similar to 0.3 degrees C/Ma) and Early Miocene enhanced cooling (similar to 2-3 degrees C/Ma) along deep valleys at the southern edge of the landscape. Given the subdued Late Jurassic to Early Cretaceous crustal deformation in the study area, we relate the coeval cooling to crustal refrigeration and exhumation triggered by northward subduction of the Meso-Tethys Ocean along the Bangong suture. Subsequent Late Cretaceous to Cenozoic minimal cooling supports arguments for the formation of a low-elevation landform prior to uplift of the southeastern TP. The enhanced cooling commenced at the Early Miocene (similar to 15-22Ma) along deep valleys and heralded the onset of river incision and surface uplift of the southeastern TP. This finding does not support previous proposals claiming that high elevations of the southeastern TP were formed in Late Miocene time resulting from lower crustal flow but rather supports a model highlighting continental subduction and extrusion along the large Tanggula-Yushu-Batang-Red River fault system.
WOS关键词INDIA-ASIA COLLISION ; EAST-CENTRAL TIBET ; RIVER SHEAR ZONE ; APATITE (U-TH)/HE THERMOCHRONOMETRY ; LOW-TEMPERATURE THERMOCHRONOMETRY ; FISSION-TRACK THERMOCHRONOLOGY ; MESOZOIC TECTONIC EVOLUTION ; SHALLOW-ANGLE SUBDUCTION ; SHAN FORELAND BASIN ; YIDUN ARC
WOS研究方向Geochemistry & Geophysics
语种英语
出版者AMER GEOPHYSICAL UNION
WOS记录号WOS:000333033400040
资助机构China National Oil-Gas Major Special Projects(2011ZX05008-002) ; China National Oil-Gas Major Special Projects(2011ZX05008-002) ; IPRS ; IPRS ; MIRS ; MIRS ; University of Melbourne ; University of Melbourne ; China National Oil-Gas Major Special Projects(2011ZX05008-002) ; China National Oil-Gas Major Special Projects(2011ZX05008-002) ; IPRS ; IPRS ; MIRS ; MIRS ; University of Melbourne ; University of Melbourne ; China National Oil-Gas Major Special Projects(2011ZX05008-002) ; China National Oil-Gas Major Special Projects(2011ZX05008-002) ; IPRS ; IPRS ; MIRS ; MIRS ; University of Melbourne ; University of Melbourne ; China National Oil-Gas Major Special Projects(2011ZX05008-002) ; China National Oil-Gas Major Special Projects(2011ZX05008-002) ; IPRS ; IPRS ; MIRS ; MIRS ; University of Melbourne ; University of Melbourne
内容类型期刊论文
源URL[http://ir.iggcas.ac.cn/handle/132A11/86688]  
专题中国科学院地质与地球物理研究所
通讯作者Tian, Yuntao
作者单位1.Univ Melbourne, Sch Earth Sci, Melbourne, Vic, Australia
2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China
推荐引用方式
GB/T 7714
Tian, Yuntao,Kohn, Barry P.,Gleadow, Andrew J. W.,et al. A thermochronological perspective on the morphotectonic evolution of the southeastern Tibetan Plateau[J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,2014,119(1):676-698.
APA Tian, Yuntao,Kohn, Barry P.,Gleadow, Andrew J. W.,&Hu, Shengbiao.(2014).A thermochronological perspective on the morphotectonic evolution of the southeastern Tibetan Plateau.JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,119(1),676-698.
MLA Tian, Yuntao,et al."A thermochronological perspective on the morphotectonic evolution of the southeastern Tibetan Plateau".JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH 119.1(2014):676-698.
个性服务
查看访问统计
相关权益政策
暂无数据
收藏/分享
所有评论 (0)
暂无评论
 

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。


©版权所有 ©2017 CSpace - Powered by CSpace