Initial Deformation of the Northern Tibetan Plateau: Insights From Deposition of the Lulehe Formation in the Qaidam Basin
Cheng, Feng3,4; Garzione, Carmala N.3; Jolivet, Marc5; Guo, Zhaojie1; Zhang, Daowei2; Zhang, Changhao2; Zhang, Qiquan2
刊名TECTONICS
2019-02-01
卷号38期号:2页码:741-766
关键词Paleogene Qaidam basin Tibetan plateau Lulehe Formation flexural loading estimate basin analysis
ISSN号0278-7407
DOI10.1029/2018TC005214
通讯作者Cheng, Feng(cfcf.chengfeng@gmail.com)
英文摘要The Paleogene Lulehe Formation marks the onset of deposition in the Qaidam basin and preserves evidence of the initial topographic growth of northern Tibet. However, limited outcrops impede understanding of the sedimentary features of the Lulehe Formation as well as the tectonic relationship between the basin and surrounding topography. To fill this gap, we investigated core samples along the basin margin and conducted flexural modeling to estimate the topographic load of the Qilian Shan and Eastern Kunlun Shan during the deposition of the Lulehe Formation. Core samples reveal that the Lulehe Formation mainly consists of distal fluvial to marginal lacustrine deposits and proximal fluvial deposits along the southern margin of the basin while characterized by proximal alluvial fan deposits along the northern margin of the basin. Together with evidence for faulting shown on the seismic profiles, we infer that simultaneous deformation within the Qilian Shan and Altyn Tagh Shan during the Paleogene resulted in accumulation of coarse detrital deposits in the northwestern and northeastern Qaidam basin. The simultaneous deformation within the Altyn Tagh Shan and Qilian Shan since the Paleogene supports the idea that deformation in these two regions is kinematically linked. One- and two-load beam flexural modeling indicates that the topographic load generated by both the Eastern Kunlun Shan and the Qilian Shan is responsible for the subsidence of the Qaidam basin during deposition of the Lulehe Formation. Our results highlight the initial relative high topography in the northern Tibetan plateau during the early Cenozoic.
资助项目National Science Foundation[EAR-1348005] ; National Science Foundation[OISE-1545859] ; National Science and Technology Major Project of China[2017ZX05008-001] ; State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences[SKLLQG1701]
WOS关键词ALTYN-TAGH FAULT ; CENOZOIC TECTONIC EVOLUTION ; INDIA-ASIA COLLISION ; EARLY UPLIFT HISTORY ; EASTERN QILIAN SHAN ; U-PB GEOCHRONOLOGY ; KUNLUN FAULT ; CONTINENTAL DEFORMATION ; HEXI CORRIDOR ; RESERVOIR CHARACTERISTICS
WOS研究方向Geochemistry & Geophysics
语种英语
出版者AMER GEOPHYSICAL UNION
WOS记录号WOS:000462017800016
资助机构National Science Foundation ; National Science and Technology Major Project of China ; State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences
内容类型期刊论文
源URL[http://ir.ieecas.cn/handle/361006/14203]  
专题地球环境研究所_黄土与第四纪地质国家重点实验室(2010~)
通讯作者Cheng, Feng
作者单位1.Peking Univ, Sch Earth & Space Sci, Key Lab Orogen Belts & Crustal Evolut, Minist Educ, Beijing, Peoples R China
2.PetroChina, Qinghai Oilfield Co, Dunhuang, Gansu, Peoples R China
3.Univ Rochester, Dept Earth & Environm Sci, Rochester, NY 14627 USA
4.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian, Shaanxi, Peoples R China
5.Univ Rennes 1, CNRS, Lab Geosci Rennes, Observ Sci Univers,UMR6118, Rennes, France
推荐引用方式
GB/T 7714
Cheng, Feng,Garzione, Carmala N.,Jolivet, Marc,et al. Initial Deformation of the Northern Tibetan Plateau: Insights From Deposition of the Lulehe Formation in the Qaidam Basin[J]. TECTONICS,2019,38(2):741-766.
APA Cheng, Feng.,Garzione, Carmala N..,Jolivet, Marc.,Guo, Zhaojie.,Zhang, Daowei.,...&Zhang, Qiquan.(2019).Initial Deformation of the Northern Tibetan Plateau: Insights From Deposition of the Lulehe Formation in the Qaidam Basin.TECTONICS,38(2),741-766.
MLA Cheng, Feng,et al."Initial Deformation of the Northern Tibetan Plateau: Insights From Deposition of the Lulehe Formation in the Qaidam Basin".TECTONICS 38.2(2019):741-766.
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