中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
The Tunggurian stage of the continental Miocene in China

文献类型:期刊论文

作者Deng Tao; Hou Sukuan; Wang Hongjiang; dengtao@ivpp.ac.cn
刊名ACTA GEOL SIN-ENGL
出版日期2007
卷号81期号:5
关键词Northern Tibetan Plateau Hispanotherium-matritense Middle Miocene Linxia Basin Neogene Gansu Biostratigraphy Subdivision Sequence Spain
ISSN号1000-9515
英文摘要The Tunggurian Age was nominated in 1984, and the Second National Commission on Stratigraphy of China formally suggested establishing the corresponding chronostratigraphic unit, the Tunggurian Stage, based on the Tunggurian Age in 1999. The name of this stage comes from a lithostratigraphic unit, the Tunggur Formation, and the stratotype section is located at the Tunggur tableland, 15 km southeast of Saihan Gobi Township, Sonid Left Banner, Inner Mongolia. The Tunggurian Age is correlated to the Astaracian of the European land mammal ages, and they share the same definition of the lower boundary at the base of the paleomagnetic Chron C5Bn.1r with an age of 15.0 Ma. In the Tairum Nor section on the southeastern edge of the Tunggur tableland, this boundary is situated within the successive deposits of reddish-brown massive mudstone of the lower part of the Tunggur Formation, with a distance of 7.6 m from the base of the grayish-white sandstones in the middle part of the section. The Tunggurian is approximately correlated to the upper part of the marine Langhian and the marine Serravallian in the International Stratigraphical Chart. The Tunggurian Stage includes two Neogene mammal faunal units, i.e. NMU 6 (MN 6) and NMU 7 (MN 7/8). The Tairum Nor fauna from the Tairum Nor section corresponds to NMU 6, and the Tunggur fauna (senso stricto) from the localities on the northwestern edge of the Tunggur tableland, such as Platybelodon Quarry, Wolf Camp and Moergen, corresponds to NMU 7. Among the Middle Miocene mammalian faunas in China, the Laogou fauna from the Linxia Basin, Gansu, the Quantougou fauna from the Lanzhou Basin, Gansu, the Halamagai fauna from the northern Junggar Basin, Xinjiang, and the Dingjiaergou fauna from Tongxin, Ningxia correspond to NMU 6.
公开日期2013-11-27
源URL[http://119.78.100.205/handle/311034/4886]  
专题古脊椎动物与古人类研究所_图书馆1
通讯作者dengtao@ivpp.ac.cn
推荐引用方式
GB/T 7714
Deng Tao,Hou Sukuan,Wang Hongjiang,et al. The Tunggurian stage of the continental Miocene in China[J]. ACTA GEOL SIN-ENGL,2007,81(5).
APA Deng Tao,Hou Sukuan,Wang Hongjiang,&dengtao@ivpp.ac.cn.(2007).The Tunggurian stage of the continental Miocene in China.ACTA GEOL SIN-ENGL,81(5).
MLA Deng Tao,et al."The Tunggurian stage of the continental Miocene in China".ACTA GEOL SIN-ENGL 81.5(2007).

入库方式: OAI收割

来源:古脊椎动物与古人类研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。