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中国陆相中新统谢家阶
引用本文:邓涛,王伟铭,岳乐平.中国陆相中新统谢家阶[J].地层学杂志,2006,30(4):315-322.
作者姓名:邓涛  王伟铭  岳乐平
作者单位:1. 中国科学院古脊椎动物与古人类研究所,北京,100044
2. 中国科学院南京地质古生物研究所,江苏南京,210008
3. 西北大学地质系,陕西西安,710069
基金项目:全国地层委员会中国新近系地层建阶研究项目,国家自然科学基金重点项目(No.40232023),国家重点基础研究发展规划项目(2006CB806400)资助。
摘    要:谢家期一名最初在1984年提出,1999年第二届全国地层委员会正式提出依据谢家期建立对应的年代地层单位——谢家阶,阶名源自同名岩石地层单位谢家组。谢家阶的层型剖面在青海省湟中县田家寨乡谢家村北1km处的车头沟,谢家阶对应于国际地层表中的海相Aquitanian阶,其共同的底界定义为古地磁ChronC6Cn.2n的底界,年龄为23.0Ma。古地磁研究结果显示在谢家剖面谢家阶的底界位于马哈拉沟组上部的棕红色块状泥岩连续沉积中,距上覆的谢家组底48m。生物地层学的综合分析表明谢家阶包含3个哺乳动物群单位,即NMU1—3。谢家剖面上发现的谢家动物群相当于NMU2,新疆准噶尔盆地北缘的索索泉动物群和甘肃兰州盆地的张家坪动物群分别相当于NMU1和NMU3。

关 键 词:谢家阶  中新统  层型剖面  生物标志  古地磁年龄  中国
文章编号:0253-4959(2006)04-0315-08
收稿时间:05 15 2006 12:00AM
修稿时间:05 30 2006 12:00AM

THE XIEJIAN STAGE OF THE CONTINENTAL MIOCENE SERIES IN CHINA
DENG Tao,WANG Wei-ming,YUE Le-ping.THE XIEJIAN STAGE OF THE CONTINENTAL MIOCENE SERIES IN CHINA[J].Journal of Stratigraphy,2006,30(4):315-322.
Authors:DENG Tao  WANG Wei-ming  YUE Le-ping
Abstract:The Xiejian Age was named in 1984, and the Second National Commission on Stratigraphy of China formally recommended in 1999 to establish the corresponding chronostratigraphic unit Xiejian Stage based on the Xiejian Age, which was named after the lithostratigraphic unit Xiejia Formation. In this paper, we propose the Chetougou section, 1 km to the north of the Xiejia village, Tianjiazhai Township, Huangzhong County, Qinghai Province, as the stratotype section of the Xiejian Stage. The Xiejian Stage can be correlated with the marine Aquitanian Stage in the International Stratigraphic Chart, and the lower boundary of both stages is defined at the base of the paleomagnetic Chron C6Cn.2n with an age of 23.0Ma . At the Xiejia section, paleomagnetic data indicate that the lower boundary of the Xiejian Stage is located within the successive deposits of reddish brown massive mudstone in the upper part of the Mahalagou Formation, about 48 m from the base of the overlying Xiejia Formation. Biostratigraphic analyses suggest that the Xiejian Stage includes three Neogene mammal faunal units, NMU 1 to NMU 3. The Xie- jia fauna discovered from the Xiejia section is regarded as NMU 2, and the Suosuoquan fauna from the northern Junggar Basin, Xinjiang, and the Zhangjiaping fauna from the Lanzhou Basin, Gansu correspond to NMU 1 and NMU 3, respectively.
Keywords:Xiejian Stage  Miocene  stratotype  biostratigraphic unit  paleomagnetic age  China
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