Magnetostratigraphy and paleoenvironmental record of Tertiary deposits of Lanzhou Basin
文献类型：期刊论文
| 作者 | Yue, LP; Heller, F; Qiu, ZX ; Zhang, L; Xie, GP; Qiu, ZD; Zhang, YX; Yue, LP (reprint author), NW Univ Xian, Dept Geol, Xian 710069, Peoples R China.
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| 刊名 | CHINESE SCIENCE BULLETIN
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| 出版日期 | 2001-05-01 |
| 卷号 | 46期号:9页码:770-774 |
| 关键词 | Paleomagnetic Stratigraphy Lanzhou Basin Tertiary The Tibetan Plateau Paleoenvironment |
| ISSN号 | 1001-6538 |
| 文献子类 | Article |
| 英文摘要 | The Tertiary deposits of the Yongdeng section, the Lanzhou Basin were studied by means of magnetostratigraphy. The magnetostratigraphic sequences from Paleocene to Miocene mere established, and the time scale for the corresponding stratigraphy and mammalian faunas was also established by referring to their correlation to the GPTS of BKSA95 (The geomagnetic polarity time scale which was thoroughly revised and updated by Berggreen et al, in 1995). In the end the paleoenvironmental records and their relationship with the uplifting of the Tibetan Plateau were dis cussed. The results are as follows. The top boundary of the Xiliugou Formation is dated to be 51 Ma, i.e. Eocene. The Yehucheng Formation covers the time span of 51-31.5 Ma, i.e, from late Early Eocene to early Early Oligocene. The Xianshuihe Formation covers the time span of 31.5-15 Ma, i.e. from Early Oligocene to Middle Miocene. The lower member of the Xianshnihe Formation spans from 31.5 to 20.0 Ma, i.e. from Early Oligocene to early Early Miocene. The middle member is from 20.0 to 16.5 Ma, i.e. in the middle Early Miocene.; The Tertiary deposits of the Yongdeng section, the Lanzhou Basin were studied by means of magnetostratigraphy. The magnetostratigraphic sequences from Paleocene to Miocene mere established, and the time scale for the corresponding stratigraphy and mammalian faunas was also established by referring to their correlation to the GPTS of BKSA95 (The geomagnetic polarity time scale which was thoroughly revised and updated by Berggreen et al, in 1995). In the end the paleoenvironmental records and their relationship with the uplifting of the Tibetan Plateau were dis cussed. The results are as follows. The top boundary of the Xiliugou Formation is dated to be 51 Ma, i.e. Eocene. The Yehucheng Formation covers the time span of 51-31.5 Ma, i.e, from late Early Eocene to early Early Oligocene. The Xianshuihe Formation covers the time span of 31.5-15 Ma, i.e. from Early Oligocene to Middle Miocene. The lower member of the Xianshnihe Formation spans from 31.5 to 20.0 Ma, i.e. from Early Oligocene to early Early Miocene. The middle member is from 20.0 to 16.5 Ma, i.e. in the middle Early Miocene. |
| WOS关键词 | TIBETAN PLATEAU |
| WOS研究方向 | Science & Technology - Other Topics |
| 语种 | 英语 |
| WOS记录号 | WOS:000169054600018 |
| 公开日期 | 2013-11-27 |
| 源URL | [http://119.78.100.205/handle/311034/3870]  |
| 专题 | 古脊椎动物与古人类研究所_图书馆1 古脊椎动物与古人类研究所_古哺乳动物研究室 |
| 通讯作者 | Yue, LP (reprint author), NW Univ Xian, Dept Geol, Xian 710069, Peoples R China. |
| 作者单位 | 1.NW Univ Xian, Dept Geol, Xian 710069, Peoples R China 2.ETH Honggerberg, Inst Geophys, CH-8093 Zurich, Switzerland 3.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China 4.Prov Museum Gansu, Lanzhou 730050, Peoples R China |
| 推荐引用方式 GB/T 7714 | Yue, LP,Heller, F,Qiu, ZX,et al. Magnetostratigraphy and paleoenvironmental record of Tertiary deposits of Lanzhou Basin[J]. CHINESE SCIENCE BULLETIN,2001,46(9):770-774. |
| APA | Yue, LP.,Heller, F.,Qiu, ZX.,Zhang, L.,Xie, GP.,...&Yue, LP .(2001).Magnetostratigraphy and paleoenvironmental record of Tertiary deposits of Lanzhou Basin.CHINESE SCIENCE BULLETIN,46(9),770-774. |
| MLA | Yue, LP,et al."Magnetostratigraphy and paleoenvironmental record of Tertiary deposits of Lanzhou Basin".CHINESE SCIENCE BULLETIN 46.9(2001):770-774. |
入库方式： OAI收割
来源：古脊椎动物与古人类研究所
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