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DOI | 10.1029/2018JB015753 |
Paleomagnetic Rotation Constraints on the Deformation of the Northern Qaidam Marginal Thrust Belt and Implications for Strike-Slip Faulting Along the Altyn Tagh Fault | |
Li, Bingshuai; Yan, Maodu; Zhang, Weilin; Fang, Xiaomin; Yang, Yongpeng; Zhang, Dawen; Chen, Yi; Guan, Chong | |
通讯作者 | Yan, MD (通讯作者) |
发表日期 | 2018 |
ISSN | 2169-9313 |
EISSN | 2169-9356 |
起始页码 | 7207 |
结束页码 | 7224 |
卷号 | 123期号:9 |
英文摘要 | Discordant Cenozoic paleomagnetic rotation results obtained throughout the northeastern Tibetan Plateau have yielded different tectonic models for the evolution of the Altyn Tagh Fault and the northeastern Tibetan Plateau. Here based on detailed existing magnetostratigraphic age constraints, we carried out an in-depth paleomagnetic study along the Hongliugou section in the middle northern Qaidam marginal thrust belt to address the Cenozoic rotations of this region. A total of 1,342 Jurassic-Neogene siltstone-sandstone core samples were collected from 128 sites across 18 time intervals. Rock magnetic analysis suggested that magnetite and hematite are the dominant magnetic carriers. Detailed thermal demagnetization analyses were performed, and the characteristic remanent magnetizations of 90 sites (743 samples) were obtained, which yielded positive fold and reversals tests, indicating that they likely represent primary magnetizations. Detailed paleomagnetic declination versus age analyses revealed three periods of rotations: 12.515.7 degrees statistically insignificant counterclockwise rotations during 45-33Ma, successive clockwise rotations of 32.215.4 degrees during 33-14Ma, and subsequent statistically insignificant counterclockwise rotations of 8.79.4 degrees after 14Ma. These three periods of rotations are similar to those calculated based on previously available magnetostratigraphic data from the nearby Dahonggou section. Based on the integration of these data with other lines of geological evidence, we attributed the latter two periods of rotations to fast strike-slip faulting along the Altyn Tagh Fault. |
关键词 | APATITE FISSION-TRACKCENOZOIC TECTONIC EVOLUTIONNE TIBETAN PLATEAUU-PB GEOCHRONOLOGYQILIAN-SHANNORTHEASTERN MARGINFOLD TESTBASIN IMPLICATIONSMIOCENE SEDIMENTSNORTHWEST CHINA |
英文关键词 | Cenozoic; paleomagnetic rotations; Altyn Tagh Fault; northern Qaidam marginal thrust belt |
语种 | 英语 |
WOS研究方向 | Geochemistry & Geophysics |
WOS类目 | Geochemistry & Geophysics |
WOS记录号 | WOS:000447858800001 |
来源期刊 | JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
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来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/259216 |
推荐引用方式 GB/T 7714 | Li, Bingshuai,Yan, Maodu,Zhang, Weilin,et al. Paleomagnetic Rotation Constraints on the Deformation of the Northern Qaidam Marginal Thrust Belt and Implications for Strike-Slip Faulting Along the Altyn Tagh Fault[J]. 中国科学院青藏高原研究所,2018,123(9). |
APA | Li, Bingshuai.,Yan, Maodu.,Zhang, Weilin.,Fang, Xiaomin.,Yang, Yongpeng.,...&Guan, Chong.(2018).Paleomagnetic Rotation Constraints on the Deformation of the Northern Qaidam Marginal Thrust Belt and Implications for Strike-Slip Faulting Along the Altyn Tagh Fault.JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,123(9). |
MLA | Li, Bingshuai,et al."Paleomagnetic Rotation Constraints on the Deformation of the Northern Qaidam Marginal Thrust Belt and Implications for Strike-Slip Faulting Along the Altyn Tagh Fault".JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH 123.9(2018). |
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