中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Paleomagnetism of the Yuanmou Basin near the southeastern margin of the Tibetan Plateau and its constraints on late Neogene sedimentation and tectonic rotation

文献类型:期刊论文

作者Zhu, R. X.1; Potts, R.2; Pan, Y. X.1; Lue, L. Q.1; Yao, H. T.1; Deng, C. L.1; Qin, H. F.1
刊名EARTH AND PLANETARY SCIENCE LETTERS
出版日期2008-07-30
卷号272期号:1-2页码:97-104
关键词Yuanmou basin magnetostratigraphy vertical-axis rotation late Neogene
ISSN号0012-821X
DOI10.1016/j.epsl.2008.04.016
文献子类Article
英文摘要New paleomagnetic investigation was carried out on the late Neogene fluviolacustrine sequence of the Yuanmou Basin, located near the southeastern margin of the Tibetan Plateau. Magnetostratigraphic results indicate nine reverse magnetozones (R1 to R9) and eight normal magnetozones (NI to N8) in the sedimentary profile, which can be correlated to the geomagnetic polarity timescale from C3n.3r to C1 r.1r. The age of the sedimentary sequence of the Yuanmou Basin can thus be paleomagnetically constrained to an interval from early Pliocene to Pleistocene, with sedimentation rates varying from 12.5 to 55 cm/kyr. In addition to its highly resolved rnagnetostratigraphic sequence, the Yuanmou Basin provides a record of Plio-Pleistocene tectono- and climato-sedimentary processes. The mean declinations of the seventeen polarity units (excluding samples with transitional directions) can be grouped into three distinct directional intervals, Group I (2.58-1.37 Ma), Group II (4.29-2.58 Ma) and Group III(4.91-4.29 Ma). These directions indicate that the Yuanmou Basin has probably experienced vertical-axis clockwise rotation of about 12 degrees from 1.4 Ma to 4.9 Ma, which may be related to slip activity of the Red River fault to the southwest and the Xianshuihe-Xiaojiang fault to the east. (C) 2008 Elsevier B.V. All rights reserved.
WOS关键词CENTRAL-ASIA ; MAGNETIC-SUSCEPTIBILITY ; NORTHERN-HEMISPHERE ; CRETACEOUS ROCKS ; EASTERN TIBET ; QAIDAM BASIN ; INDO-CHINA ; MYR AGO ; DEFORMATION ; UPLIFT
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000259119900010
出版者ELSEVIER SCIENCE BV
资助机构NSFC(40221402) ; NSFC(40221402) ; CAS ; CAS ; U.S. National Science Foundation((BCS 0218511)) ; U.S. National Science Foundation((BCS 0218511)) ; Smithsonian's Human Origins Program ; Smithsonian's Human Origins Program ; NSFC(40221402) ; NSFC(40221402) ; CAS ; CAS ; U.S. National Science Foundation((BCS 0218511)) ; U.S. National Science Foundation((BCS 0218511)) ; Smithsonian's Human Origins Program ; Smithsonian's Human Origins Program ; NSFC(40221402) ; NSFC(40221402) ; CAS ; CAS ; U.S. National Science Foundation((BCS 0218511)) ; U.S. National Science Foundation((BCS 0218511)) ; Smithsonian's Human Origins Program ; Smithsonian's Human Origins Program ; NSFC(40221402) ; NSFC(40221402) ; CAS ; CAS ; U.S. National Science Foundation((BCS 0218511)) ; U.S. National Science Foundation((BCS 0218511)) ; Smithsonian's Human Origins Program ; Smithsonian's Human Origins Program
源URL[http://ir.iggcas.ac.cn/handle/132A11/68970]  
专题中国科学院地质与地球物理研究所
通讯作者Zhu, R. X.
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Paleomagnetism & Geochronol Lab SKL LE, Beijing 100029, Peoples R China
2.Smithsonian Inst, Natl Museum Nat Hist, Human Origins Program, Washington, DC 20013 USA
推荐引用方式
GB/T 7714
Zhu, R. X.,Potts, R.,Pan, Y. X.,et al. Paleomagnetism of the Yuanmou Basin near the southeastern margin of the Tibetan Plateau and its constraints on late Neogene sedimentation and tectonic rotation[J]. EARTH AND PLANETARY SCIENCE LETTERS,2008,272(1-2):97-104.
APA Zhu, R. X..,Potts, R..,Pan, Y. X..,Lue, L. Q..,Yao, H. T..,...&Qin, H. F..(2008).Paleomagnetism of the Yuanmou Basin near the southeastern margin of the Tibetan Plateau and its constraints on late Neogene sedimentation and tectonic rotation.EARTH AND PLANETARY SCIENCE LETTERS,272(1-2),97-104.
MLA Zhu, R. X.,et al."Paleomagnetism of the Yuanmou Basin near the southeastern margin of the Tibetan Plateau and its constraints on late Neogene sedimentation and tectonic rotation".EARTH AND PLANETARY SCIENCE LETTERS 272.1-2(2008):97-104.

入库方式: OAI收割

来源:地质与地球物理研究所

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