Tectonic and sedimentary evolution of the late Miocene-Pleistocene Dali Basin in the southeast margin of the Tibetan Plateau: Evidences from anisotropy of magnetic susceptibility and rock magnetic data | |
Li, Shihu1; Deng, Chenglong1; Paterson, Greig A.2; Yao, Haitao3; Huang, Sheng1; Liu, Chengying1; He, Huaiyu2; Pan, Yongxin2; Zhu, Rixiang1 | |
刊名 | TECTONOPHYSICS
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2014-08-26 | |
卷号 | 629页码:362-377 |
关键词 | Anisotropy of magnetic susceptibility Dali Basin Southeast margin of the Tibetan Plateau Dali fault system |
ISSN号 | 0040-1951 |
DOI | 10.1016/j.tecto.2014.05.035 |
文献子类 | Article |
英文摘要 | The Cenozoic Dali Basin, located at the northeast of Diancang Shan and south of the first bend of Yangtze River, is tectonically controlled by the Dali fault system in the southeast margin of the Tibetan Plateau. The basin is filled with late Miocene to Pleistocene fluviolacustrine sediments, which provide invaluable information about the tectonic deformation and drainage network reorganization in this area. In this study, we discuss the anisotropy of magnetic susceptibility (AMS) of the Dasongping section in the Dali Basin, which spans an interval from 7.6 to 1.8 Ma. Although rock magnetic experiments indicate that magnetite and hematite are the main remanence carriers, hysteresis loops, low values of bulk susceptibility and low temperature susceptibility suggest that paramagnetic minerals are major contributors to low-field AMS. The rock magnetic parameters indicate that the Dali Basin experienced four stages of infilling and the sediment sources may have changed at 4.2 Ma. The clustering of the minimum principle axes (K-min) nearly perpendicular to the bedding plane and the pronounced N-S magnetic lineation parallel to the bedding plane indicate that the AMS of the Dali Basin is a superimposed fabric consisting of a sedimentary-compaction and a mild initial deformation overprint. The well-defined N-S magnetic lineation is likely due to the NNW and NNE oblique shear caused by the Heqing and Red River faults. (C) 2014 Elsevier B.V. All rights reserved. |
WOS关键词 | LOWER-CRUSTAL FLOW ; SHEAR ZONE ; RED-RIVER ; UNDEFORMED CLAYS ; TARIM BASIN ; EXTENSIONAL TECTONICS ; NEUTRON TEXTURE ; CENOZOIC UPLIFT ; WESTERN YUNNAN ; SURFACE UPLIFT |
WOS研究方向 | Geochemistry & Geophysics |
语种 | 英语 |
出版者 | ELSEVIER SCIENCE BV |
WOS记录号 | WOS:000341474600029 |
资助机构 | China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; National Key Basic Research Program of China(2012CB821900) ; National Key Basic Research Program of China(2012CB821900) ; National Key Basic Research Program of China(2012CB821900) ; National Key Basic Research Program of China(2012CB821900) ; Chinese Academy of Sciences(KZCX2-YW-Q05-02 ; Chinese Academy of Sciences(KZCX2-YW-Q05-02 ; Chinese Academy of Sciences(KZCX2-YW-Q05-02 ; Chinese Academy of Sciences(KZCX2-YW-Q05-02 ; National Natural Science Foundation of China(20811240 ; National Natural Science Foundation of China(20811240 ; National Natural Science Foundation of China(20811240 ; National Natural Science Foundation of China(20811240 ; KZCX2-EW-117) ; KZCX2-EW-117) ; KZCX2-EW-117) ; KZCX2-EW-117) ; 41274073 ; 41274073 ; 41274073 ; 41274073 ; 40925012 ; 40925012 ; 40925012 ; 40925012 ; 41174054) ; 41174054) ; 41174054) ; 41174054) ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; National Key Basic Research Program of China(2012CB821900) ; National Key Basic Research Program of China(2012CB821900) ; National Key Basic Research Program of China(2012CB821900) ; National Key Basic Research Program of China(2012CB821900) ; Chinese Academy of Sciences(KZCX2-YW-Q05-02 ; Chinese Academy of Sciences(KZCX2-YW-Q05-02 ; Chinese Academy of Sciences(KZCX2-YW-Q05-02 ; Chinese Academy of Sciences(KZCX2-YW-Q05-02 ; National Natural Science Foundation of China(20811240 ; National Natural Science Foundation of China(20811240 ; National Natural Science Foundation of China(20811240 ; National Natural Science Foundation of China(20811240 ; KZCX2-EW-117) ; KZCX2-EW-117) ; KZCX2-EW-117) ; KZCX2-EW-117) ; 41274073 ; 41274073 ; 41274073 ; 41274073 ; 40925012 ; 40925012 ; 40925012 ; 40925012 ; 41174054) ; 41174054) ; 41174054) ; 41174054) ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; National Key Basic Research Program of China(2012CB821900) ; National Key Basic Research Program of China(2012CB821900) ; National Key Basic Research Program of China(2012CB821900) ; National Key Basic Research Program of China(2012CB821900) ; Chinese Academy of Sciences(KZCX2-YW-Q05-02 ; Chinese Academy of Sciences(KZCX2-YW-Q05-02 ; Chinese Academy of Sciences(KZCX2-YW-Q05-02 ; Chinese Academy of Sciences(KZCX2-YW-Q05-02 ; National Natural Science Foundation of China(20811240 ; National Natural Science Foundation of China(20811240 ; National Natural Science Foundation of China(20811240 ; National Natural Science Foundation of China(20811240 ; KZCX2-EW-117) ; KZCX2-EW-117) ; KZCX2-EW-117) ; KZCX2-EW-117) ; 41274073 ; 41274073 ; 41274073 ; 41274073 ; 40925012 ; 40925012 ; 40925012 ; 40925012 ; 41174054) ; 41174054) ; 41174054) ; 41174054) ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; National Key Basic Research Program of China(2012CB821900) ; National Key Basic Research Program of China(2012CB821900) ; National Key Basic Research Program of China(2012CB821900) ; National Key Basic Research Program of China(2012CB821900) ; Chinese Academy of Sciences(KZCX2-YW-Q05-02 ; Chinese Academy of Sciences(KZCX2-YW-Q05-02 ; Chinese Academy of Sciences(KZCX2-YW-Q05-02 ; Chinese Academy of Sciences(KZCX2-YW-Q05-02 ; National Natural Science Foundation of China(20811240 ; National Natural Science Foundation of China(20811240 ; National Natural Science Foundation of China(20811240 ; National Natural Science Foundation of China(20811240 ; KZCX2-EW-117) ; KZCX2-EW-117) ; KZCX2-EW-117) ; KZCX2-EW-117) ; 41274073 ; 41274073 ; 41274073 ; 41274073 ; 40925012 ; 40925012 ; 40925012 ; 40925012 ; 41174054) ; 41174054) ; 41174054) ; 41174054) |
内容类型 | 期刊论文 |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/86347] ![]() |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Li, Shihu |
作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Earth & Planetary Phys, Beijing 100029, Peoples R China 3.Chinese Acad Geol Sci, Inst Geomech, Beijing 100081, Peoples R China |
推荐引用方式 GB/T 7714 | Li, Shihu,Deng, Chenglong,Paterson, Greig A.,et al. Tectonic and sedimentary evolution of the late Miocene-Pleistocene Dali Basin in the southeast margin of the Tibetan Plateau: Evidences from anisotropy of magnetic susceptibility and rock magnetic data[J]. TECTONOPHYSICS,2014,629:362-377. |
APA | Li, Shihu.,Deng, Chenglong.,Paterson, Greig A..,Yao, Haitao.,Huang, Sheng.,...&Zhu, Rixiang.(2014).Tectonic and sedimentary evolution of the late Miocene-Pleistocene Dali Basin in the southeast margin of the Tibetan Plateau: Evidences from anisotropy of magnetic susceptibility and rock magnetic data.TECTONOPHYSICS,629,362-377. |
MLA | Li, Shihu,et al."Tectonic and sedimentary evolution of the late Miocene-Pleistocene Dali Basin in the southeast margin of the Tibetan Plateau: Evidences from anisotropy of magnetic susceptibility and rock magnetic data".TECTONOPHYSICS 629(2014):362-377. |
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