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Tectonic Control of a Change in Sedimentary Environment at similar to 10 Ma in the Northeastern Tibetan Plateau
Zhang, T (Zhang, Tao)1,2; Han, WX (Han, Wenxia)3; Fang, XM (Fang, Xiaomin)1,2,4; Miao, YF (Miao, Yunfa)4,5; Zhang, WL (Zhang, Weilin)1,2; Song, CH (Song, Chunhui)6,7; Wang, YD (Wang, Yadong)8; Khatri, DB (Khatri, Dhan Bahadur)1,2,4; Zhang, ZG (Zhang, Zhigao)9
Source PublicationGEOPHYSICAL RESEARCH LETTERS
2018-07-28
Volume45Issue:14Pages:6843-6852
DOI10.1029/2018GL078460
AbstractTectonic uplift and climate change play a key role in the evolution of sedimentary systems in terrestrial basins. The Qaidam Basin in the northeastern Tibetan Plateau is well suited for studying these processes because of its location and its thick, continuous sequence of Cenozoic sediments. Unfortunately, however, there is a lack of continuous, well-dated sedimentary records from the region. In the present study, we combined grain-size analyses of sediment cores and outcrop samples with structural analysis of seismostratigraphic data from the western Qaidam Basin. The results reveal dramatic shifts in the depositional environment at similar to 11.5-10Ma, coeval with the topographic development of the area. Together with paleoclimatic analysis and a conceptual model, we conclude that tectonic movements, rather than climatic changes, were the dominant forcing factor. 
WOS IDWOS:000442582100011
Language英语
Indexed BySCIE
KeywordWESTERN QAIDAM BASIN GRAIN-SIZE DISTRIBUTION MODERN CLASTIC LAKE ALTYN-TAGH FAULT MIDDLE MIOCENE CLIMATE-CHANGE DEPOSITIONAL PROCESSES CENOZOIC TECTONICS CORE SEDIMENTS GROWTH STRATA
WOS Research AreaGeology
WOS SubjectGeosciences, Multidisciplinary
Cooperation Status国内
ISSN0094-8276
Department大陆碰撞与高原隆升重点实验室
PublisherAMER GEOPHYSICAL UNION
Citation statistics
Cited Times:1[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.itpcas.ac.cn/handle/131C11/8591
Collection图书馆
Affiliation1.Chinese Acad Sci, Inst Tibetan Plateau Res, Beijing, Peoples R China;
2.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China;
3.Linyi Univ, Sch Resources & Environm Sci, Shandong Prov Key Lab Water & Soil Conservat & En, Linyi, Peoples R China;
4.Univ Chinese Acad Sci, Beijing, Peoples R China;
5.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Inst, Key Lab Desert & Desertificat, Lanzhou, Gansu, Peoples R China;
6.Lanzhou Univ, Sch Earth Sci, Lanzhou, Gansu, Peoples R China;
7.Lanzhou Univ, Key Lab Western Chinas Mineral Resources Gansu Pr, Lanzhou, Gansu, Peoples R China;
8.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resources Res, Gansu Prov Key Lab Petr Resources, Lanzhou, Gansu, Peoples R China;
9.Anyang Normal Univ, Sch Resource Environm & Tourism, Anyang, Peoples R China.
Recommended Citation
GB/T 7714
Zhang, T ,Han, WX ,Fang, XM ,et al. Tectonic Control of a Change in Sedimentary Environment at similar to 10 Ma in the Northeastern Tibetan Plateau[J]. GEOPHYSICAL RESEARCH LETTERS,2018,45(14):6843-6852.
APA Zhang, T .,Han, WX .,Fang, XM .,Miao, YF .,Zhang, WL .,...&Zhang, ZG .(2018).Tectonic Control of a Change in Sedimentary Environment at similar to 10 Ma in the Northeastern Tibetan Plateau.GEOPHYSICAL RESEARCH LETTERS,45(14),6843-6852.
MLA Zhang, T ,et al."Tectonic Control of a Change in Sedimentary Environment at similar to 10 Ma in the Northeastern Tibetan Plateau".GEOPHYSICAL RESEARCH LETTERS 45.14(2018):6843-6852.
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