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Optically Stimulated Luminescence(OSL) Chronology of the Dehenglong Landslide from Longyang Gorge to Liujia Gorge along Upper Yellow River, China

查看全文 作  者:GUO [1]Xiaohua;LAI [2]Zhongping;LU [1]Yudong;LI [3]Xiaolin;SUN [1]Zheng 高影响力作者 机构地区:[1]Key Laboratory of Subsurface Hydrology and Ecological Effect in Arid Region of Ministry of Education, School of Environmental Science and Engineering, Chang'an University;[2]School of Earth Sciences, China University of Geosciences;[3]Key Laboratory of Environmental Geology of Qinghai Province,Qinghai Provincial 906, Qinghai Institute of Geological Investigation高影响力机构 出  处:《Acta Geologica Sinica(English Edition)》索引2015年第89卷第1期,共9页高影响力期刊 基  金:supported by China NSF(grant No.41172168);Mechanism of giant landslides from Longyang Gorge to Liujia Gorge along upper Yellow River(Grant No.1212010818083) 摘  要:Giant landslides are common along the upper Yellow River from Longyang Gorge to Liujia Gorge, and some of them even blocked and dammed the upper Yellow River. Chronology is inevitable in studying the mechanism of giant landslides. Controversy exists about the chronology of those giant landslides, and some have not yet dated. The Dehenglong landslide is the largest one among them. In this study, OSL samples were collected from lacustrine silty sediments and loess directly overlying the landslide sediments, as well as fault sediments related to the landslide. This landslide yielded an age of 89 ± 8 ka, which is identical with the fault age of 73 ± 5 ka at two sigma errors. The agreement of a topographic analysis and the absolute age of landslides imply that the formation of the Dehenglong landslide is strongly correlated with the tectonic activity. 关 键 词:巨型滑坡 黄河上游 刘家峡 龙羊峡 OSL 年表 光释光 湖泊沉积物
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