Evidence for northeastern Tibetan Plateau uplift between 25 and 20 Ma in the sedimentary archive of the Xining Basin, Northwestern China
文献类型:期刊论文
作者 | Hao, QZ (Hao, Qingzhen)[3]; Wu, NQ (Wu, Naiqin)[3]; Lu, HY (Lu, Houyuan)[3]; Xiao, GQ (Xiao, Guoqiao)[1,2]; Guo, ZT (Guo, Zhengtang)[3]; Dupont-Nivet, G (Dupont-Nivet, Guillaume)[4,5,6]; Zhang, KX (Zhang, Kexin)[2]; Abels, HA (Abels, Hemmo A.)[8]; Li, FJ (Li, Fengjiang)[3]; Peng, SZ (Peng, Shuzhen)[7] |
刊名 | EARTH AND PLANETARY SCIENCE LETTERS |
出版日期 | 2012-02-01 |
卷号 | 317页码:185-195 |
关键词 | Ne Tibet Magnetostratigraphy Tectonic Uplift Paleoclimate Sedimentary Provenance Xining Basin |
文献子类 | 期刊论文 |
英文摘要 | The growth history of the Tibetan Plateau provides a valuable natural laboratory to understand tectonic processes of the India-Asia collision and their impact on and interactions with Asian and global climate change. However, both Tibetan Plateau growth and Asian paleoenvironments are generally poorly documented in pre-Pliocene times and reflect limited temporal coverage for different parts of the plateau. Here we present magnetostratigraphic results from the Xining Basin, at the NE margin of the Tibetan Plateau, precisely dating the record between the earliest Oligocene (similar to 33 Ma) to the middle Miocene (similar to 16 Ma). The pattern of observed paleomagnetic polarity zones is unequivocally correlated to the geomagnetic polarity time scale (GPTS) indicating relatively constant and low sediment accumulation rates (32 m/Myr) except for a peculiar period of unstable accumulation between 25.3 and 19.7 Ma. At the beginning of this interval, a marked permanent increase in magnetite content of the sediments is observed and likely relates to a change in provenance. We directly relate this unstable period of sediment accumulation and provenance change to the coeval exhumation recently reported by low-temperature thermochronology from the Laji Shan range, which subsequently formed the southern margin of the Xining Basin. Evidence for NE Tibet tectonism at 25-20 Ma can be associated with widespread deformation over the entire Himalayan-Tibetan orogen at this time, which may be linked to the coeval appearance of monsoon climate in Eastern Asia and the onset of central Asian desertification. |
语种 | 英语 |
源URL | [http://ir.ieecas.cn/handle/361006/10121] |
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 | Guo, ZT (Guo, Zhengtang)[3] |
作者单位 | 1.Paleomagnetic Laboratory ‘Fort Hoofddijk’, Dept. of Earth Sciences, Utrecht University, Utrecht, The Netherlands; 2.State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, P.O. Box 17, Xian, 710075, China; 3.State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430074, China; 4.Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China; 5.Geociences Rennes UMR 6118-CRNS, Université de Rennes 1, Campus de Beaulieu, 35042 Rennes Cedex, France; 6.Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education (Peking Unviersity), Beijing 100871, PR China; 7.Taishan College, Tai'an 271021, China; 8.Stratigraphy/Paleontology, Dept. of Earth Sciences, Utrecht University, Utrecht, The Netherlands |
推荐引用方式 GB/T 7714 | Hao, QZ ,Wu, NQ ,Lu, HY ,et al. Evidence for northeastern Tibetan Plateau uplift between 25 and 20 Ma in the sedimentary archive of the Xining Basin, Northwestern China[J]. EARTH AND PLANETARY SCIENCE LETTERS,2012,317:185-195. |
APA | Hao, QZ .,Wu, NQ .,Lu, HY .,Xiao, GQ .,Guo, ZT .,...&Ge, JY .(2012).Evidence for northeastern Tibetan Plateau uplift between 25 and 20 Ma in the sedimentary archive of the Xining Basin, Northwestern China.EARTH AND PLANETARY SCIENCE LETTERS,317,185-195. |
MLA | Hao, QZ ,et al."Evidence for northeastern Tibetan Plateau uplift between 25 and 20 Ma in the sedimentary archive of the Xining Basin, Northwestern China".EARTH AND PLANETARY SCIENCE LETTERS 317(2012):185-195. |
入库方式: OAI收割
来源:地球环境研究所
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