中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
E/I-corrected inclination shallowing in Cenozoic redbeds from the northern Tarim Basin, NW China: Possible causes and paleogeographic implications

文献类型:期刊论文

作者Zhang, Zhiliang1,2; Shen, Bai1; Sun, Jimin2; Ren, Zhikun1
刊名GEOSPHERE
出版日期2022-03-16
页码14
ISSN号1553-040X
DOI10.1130/GES02480.1
英文摘要Because of their widespread occurrence and ability to carry stable remanence, continental redbeds in central Asia are frequently used in paleomagnetic studies. However, the paleomagnetic inclinations recorded by redbeds are much shallower than the expected values, as redbeds are usually subjected to inclination shallowing. To recognize and correct the inclinations recorded by the Cenozoic redbeds, the paleomagnetic data that were used for magnetostratigraphic studies in the Kuqa Depression, northern Tarim Basin, are reanalyzed in this study. The mean inclinations of the four groups of samples (Eocene, Oligocene, Miocene, and Pliocene) are systematically similar to 20 degrees shallower than the expected values calculated from the apparent polar wander paths (APWPs) of Eurasia, indicating the presence of inclination shallowing. We apply the elongation/inclination (E/I) method to correct the inclination shallowing. The mean inclinations of the Eocene, Oligocene, Miocene, and Pliocene sediments are corrected from 40.5 degrees to 63.1 degrees, 41.0 degrees to 63.8 degrees, 42.0 degrees to 63.8 degrees, and 44.7 degrees to 63.2 degrees, within 95% confidence limits between 55.1 degrees and 71.6 degrees, 53.7 degrees and 70.4 degrees, 51.5 degrees and 72.7 degrees, and 52.2 degrees and 71.3 degrees, respectively, which are indistinguishable from the expected inclination values. Our results suggest that inclination shallowing in the redbeds of central Asia can be reasonably corrected using the Ell method, and sedimentary processes such as compaction and/or imbrication in the very early stage of burial are important causes for inclination shallowing. Paleolatitudes calculated from the E/I-corrected inclinations show that the Tarim Basin should have reached or been at least close to its current latitude since the Cretaceous. The Cenozoic crustal shortening estimate of the northern Tarim Basin is not detectible for paleomagnetic study.
WOS关键词APPARENT POLAR WANDER ; SEDIMENTARY-ROCKS ; TIEN-SHAN ; RED BEDS ; TIAN-SHAN ; REMANENT MAGNETIZATION ; PALEOMAGNETIC INCLINATIONS ; BAICHENG DEPRESSION ; WESTERN CHINA ; ANISOTROPY
资助项目National Science and Technology Basic Resources Investi-gation Program of China[2021FY100102] ; Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration[IGCEA2113] ; Strategic Priority Research Program of Chinese Academy of Sciences[XDA20070202] ; National Nature Science Foundation of China[41888101] ; National Nature Science Foundation of China[41702209] ; National Nature Science Foundation of China[41672168]
WOS研究方向Geology
语种英语
WOS记录号WOS:000780878500001
出版者GEOLOGICAL SOC AMER, INC
资助机构National Science and Technology Basic Resources Investi-gation Program of China ; National Science and Technology Basic Resources Investi-gation Program of China ; National Science and Technology Basic Resources Investi-gation Program of China ; National Science and Technology Basic Resources Investi-gation Program of China ; Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration ; Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration ; Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration ; Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Science and Technology Basic Resources Investi-gation Program of China ; National Science and Technology Basic Resources Investi-gation Program of China ; National Science and Technology Basic Resources Investi-gation Program of China ; National Science and Technology Basic Resources Investi-gation Program of China ; Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration ; Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration ; Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration ; Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Science and Technology Basic Resources Investi-gation Program of China ; National Science and Technology Basic Resources Investi-gation Program of China ; National Science and Technology Basic Resources Investi-gation Program of China ; National Science and Technology Basic Resources Investi-gation Program of China ; Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration ; Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration ; Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration ; Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Science and Technology Basic Resources Investi-gation Program of China ; National Science and Technology Basic Resources Investi-gation Program of China ; National Science and Technology Basic Resources Investi-gation Program of China ; National Science and Technology Basic Resources Investi-gation Program of China ; Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration ; Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration ; Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration ; Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/105108]  
专题地质与地球物理研究所_中国科学院新生代地质与环境重点实验室
通讯作者Zhang, Zhiliang
作者单位1.China Earthquake Adm, Inst Geol, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Zhang, Zhiliang,Shen, Bai,Sun, Jimin,et al. E/I-corrected inclination shallowing in Cenozoic redbeds from the northern Tarim Basin, NW China: Possible causes and paleogeographic implications[J]. GEOSPHERE,2022:14.
APA Zhang, Zhiliang,Shen, Bai,Sun, Jimin,&Ren, Zhikun.(2022).E/I-corrected inclination shallowing in Cenozoic redbeds from the northern Tarim Basin, NW China: Possible causes and paleogeographic implications.GEOSPHERE,14.
MLA Zhang, Zhiliang,et al."E/I-corrected inclination shallowing in Cenozoic redbeds from the northern Tarim Basin, NW China: Possible causes and paleogeographic implications".GEOSPHERE (2022):14.

入库方式: OAI收割

来源:地质与地球物理研究所

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