Magnetostratigraphy of the Dahonggou section, northern Qaidam Basin and its bearing on Cenozoic tectonic evolution of the Qilian Shan and Altyn Tagh Fault
文献类型：期刊论文
| 作者 | Lu, Haijian; Xiong, Shangfa |
| 刊名 | EARTH AND PLANETARY SCIENCE LETTERS
 |
| 出版日期 | 2009-11-15 |
| 卷号 | 288期号:3-4页码:539-550 |
| ISSN号 | 0012-821X |
| 关键词 | Qilian Shan Altyn Tagh Fault tectonic uplift magnetostratigraphy Dahonggou section |
| DOI | 10.1016/j.epsl.2009.10.016 |
| 文献子类 | Article |
| 英文摘要 | The timing of uplift of the Tibet Plateau has a central role in the development of tectonic models for the Tibet Plateau and Cenozoic global climate change. A detailed magnetostratigraphic study of the Dahonggou section, northern Qaidam Basin, reveal that the section spans from similar to 34 to similar to 8.5 Ma and the ages of the Shang Ganchaigou, Xia Youshashan and Shang Youshashan formations are from > 34 to 22-20 Ma, 22-20 to 13 Ma and 13 to <8.5 Ma, respectively. Variations in lithofacies, sedimentation rate and magnetic susceptibility (K) suggest that the southern Qilian Shan was tectonically inactive and didn't respond to the rapid slip on the Altyn Tagh Fault at 30 Ma. In contrast, the similar sedimentary records in the Dahonggou section, the Xishuigou section along the Altyn Tagh Fault, and even more localities along much of the Qilian range front imply that the Qilian Shan and the Altyn Tagh Fault were synchronously tectonically active at about 12 Ma. The lower K between similar to 12 Ma and similar to 8.5 Ma in the sediments of the Dahonggou section is interpreted to be due to long-distanced oxidation and sorting, which cause not only that magnetite was oxidated to hematite, but also that magnetic minerals are enriched in fine-grained sediments and coarse-grained sediments bear few magnetic mineral. (C) 2009 Elsevier B.V. All rights reserved. |
| WOS关键词 | RESOLUTION MAGNETO STRATIGRAPHY ; QINGHAI-TIBET PLATEAU ; DRIVEN CLIMATE-CHANGE ; TIAN-SHAN ; WESTERN CHINA ; TARIM BASIN ; LINXIA BASIN ; NW CHINA ; CENTRAL-ASIA ; NORTHEASTERN MARGIN |
| WOS研究方向 | Geochemistry & Geophysics |
| 语种 | 英语 |
| 出版者 | ELSEVIER SCIENCE BV |
| WOS记录号 | WOS:000273150900020 |
| 资助机构 | Chinese Academy of Sciences(KZCX2-YW-130 ; Chinese Academy of Sciences(KZCX2-YW-130 ; NSF of China(40672117) ; NSF of China(40672117) ; KZCX2-YW-Q05 ; KZCX2-YW-Q05 ; KZCX2-SW-133) ; KZCX2-SW-133) ; Chinese Academy of Sciences(KZCX2-YW-130 ; Chinese Academy of Sciences(KZCX2-YW-130 ; NSF of China(40672117) ; NSF of China(40672117) ; KZCX2-YW-Q05 ; KZCX2-YW-Q05 ; KZCX2-SW-133) ; KZCX2-SW-133) ; Chinese Academy of Sciences(KZCX2-YW-130 ; Chinese Academy of Sciences(KZCX2-YW-130 ; NSF of China(40672117) ; NSF of China(40672117) ; KZCX2-YW-Q05 ; KZCX2-YW-Q05 ; KZCX2-SW-133) ; KZCX2-SW-133) ; Chinese Academy of Sciences(KZCX2-YW-130 ; Chinese Academy of Sciences(KZCX2-YW-130 ; NSF of China(40672117) ; NSF of China(40672117) ; KZCX2-YW-Q05 ; KZCX2-YW-Q05 ; KZCX2-SW-133) ; KZCX2-SW-133) |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/70734]  |
| 专题 | 中国科学院地质与地球物理研究所 |
| 通讯作者 | Lu, Haijian |
| 作者单位 | Chinese Acad Sci, Key Lab Cenozo Geol & Environm, Inst Geol & Geophys, Beijing 100029, Peoples R China |
| 推荐引用方式 GB/T 7714 | Lu, Haijian,Xiong, Shangfa. Magnetostratigraphy of the Dahonggou section, northern Qaidam Basin and its bearing on Cenozoic tectonic evolution of the Qilian Shan and Altyn Tagh Fault[J]. EARTH AND PLANETARY SCIENCE LETTERS,2009,288(3-4):539-550. |
| APA | Lu, Haijian,&Xiong, Shangfa.(2009).Magnetostratigraphy of the Dahonggou section, northern Qaidam Basin and its bearing on Cenozoic tectonic evolution of the Qilian Shan and Altyn Tagh Fault.EARTH AND PLANETARY SCIENCE LETTERS,288(3-4),539-550. |
| MLA | Lu, Haijian,et al."Magnetostratigraphy of the Dahonggou section, northern Qaidam Basin and its bearing on Cenozoic tectonic evolution of the Qilian Shan and Altyn Tagh Fault".EARTH AND PLANETARY SCIENCE LETTERS 288.3-4(2009):539-550. |
入库方式： OAI收割
来源：地质与地球物理研究所
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