High-resolution late Pliocene-quaternary magnetostratigraphy of the Yinchuan Basin, NE Tibetan Plateau
Ma, Xuedong5; Yin, Gongming4; Wei, Chuanyi4; Qiang, Xiaoke3; Ma, Yuxue5; Liu, Chunru4; Zhao, Zhipeng2; Gong, Liang5; Wang, Libin4; Ji, Hao4
刊名QUATERNARY INTERNATIONAL
2022-01-10
卷号607页码:120-127
关键词Northeastern Tibetan plateau Yinchuan basin Late pliocene-quaternary Fluvio-lacustrine sediment Magnetostratigraphy
ISSN号1040-6182
DOI10.1016/j.quaint.2021.09.009
通讯作者Wei, Chuanyi(chuanyiwei@ies.ac.cn) ; Qiang, Xiaoke(qiangxk@loess.llqg.ac.cn)
英文摘要The Yinchuan Basin, one of the most important basins in the area adjacent to the northeastern Tibetan Plateau, contains a continuous sequence of fluvio-lacustrine deposits, which makes it an ideal area to study the in-teractions between the Tibetan Plateau uplift, climate change, and geomorphological evolution. Here, a 1200-m -deep drill core (YNZK01) is described with an average recovery rate of 96% in the depo-center of the Yinchuan Basin to establish a high-resolution palaeoenvironmental and tectonic reconstruction. Stepwise alternating-field demagnetization results showed a stable and high-qualified remanent magnetization of the samples. The polarity sequences consisted of 8 normal and 8 reverse zones that correlate well with the geomagnetic polarity timescale. Magnetostratigraphic results date the entire YNZK01 core from 3.927 Ma to the present. The B/M boundary (0.781 Ma) is at a depth of 246.4 m while the M/G boundary (2.581 Ma) is at a depth of 863.4 m. The G/Gi boundary (3.596 Ma) is identified at 1117.8 m and the bottom of the core was extrapolated to 3.927 Ma (1201 m) with an average sedimentation rate of 863.4-1117.8 m. This high-resolution magnetostratigraphy record pro -vides a baseline chronological framework for further research and publications on the tectonic, paleoclimatic, and paleoenvironmental proxy data of the YNZK01 core in the Yinchuan Basin, NE Tibetan Plateau.
资助项目Ningxia Geological Exploration[HZ20170040-I] ; project of Urban geological survey in the yinchuan metropolitan area[[2017] 320] ; National Natural Science Foundation of China[41772185] ; National Nonprofit Fundamental Research Grant of China, Institute of Geology, China, Earthquake Administration[IGCEA2015] ; National Nonprofit Fundamental Research Grant of China, Institute of Geology, China, Earthquake Administration[IGCEA1908]
WOS关键词EVOLUTION ; UPLIFT ; PL02
WOS研究方向Physical Geography ; Geology
语种英语
出版者PERGAMON-ELSEVIER SCIENCE LTD
WOS记录号WOS:000718035100006
资助机构Ningxia Geological Exploration ; project of Urban geological survey in the yinchuan metropolitan area ; National Natural Science Foundation of China ; National Nonprofit Fundamental Research Grant of China, Institute of Geology, China, Earthquake Administration
内容类型期刊论文
源URL[http://ir.ieecas.cn/handle/361006/17241]  
专题地球环境研究所_古环境研究室
通讯作者Wei, Chuanyi; Qiang, Xiaoke
作者单位1.China Univ Geosci, Inst Geophys & Geomat, Wuhan 430074, Hubei, Peoples R China
2.Geol Bur Ningxia Hui Autonomous Reg, Yinchuan 750021, Ningxia, Peoples R China
3.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Shaanxi, Peoples R China
4.China Earthquake Adm, State Key Lab Earthquake Dynam, Inst Geol, Beijing 100029, Peoples R China
5.Ningxia Inst Geol Survey, Yinchuan 750021, Ningxia, Peoples R China
推荐引用方式
GB/T 7714
Ma, Xuedong,Yin, Gongming,Wei, Chuanyi,et al. High-resolution late Pliocene-quaternary magnetostratigraphy of the Yinchuan Basin, NE Tibetan Plateau[J]. QUATERNARY INTERNATIONAL,2022,607:120-127.
APA Ma, Xuedong.,Yin, Gongming.,Wei, Chuanyi.,Qiang, Xiaoke.,Ma, Yuxue.,...&Li, Guoqing.(2022).High-resolution late Pliocene-quaternary magnetostratigraphy of the Yinchuan Basin, NE Tibetan Plateau.QUATERNARY INTERNATIONAL,607,120-127.
MLA Ma, Xuedong,et al."High-resolution late Pliocene-quaternary magnetostratigraphy of the Yinchuan Basin, NE Tibetan Plateau".QUATERNARY INTERNATIONAL 607(2022):120-127.
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