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包头地区晚更新世—全新世地层划分对比及环境变迁
引用本文:邓金宪,刘正宏,徐仲元,杨振升,温泉波,李丰江,宋海峰.包头地区晚更新世—全新世地层划分对比及环境变迁[J].地层学杂志,2007,31(2):133-140.
作者姓名:邓金宪  刘正宏  徐仲元  杨振升  温泉波  李丰江  宋海峰
作者单位:吉林大学地球科学学院,吉林长春,130026
基金项目:中国地质调查局1/25万《包头幅》区域地质调查(No.200113000021).吉林大学地球科学学院刘茂修教授、赵达教授和彭向东教授参加了本次工作的野外调查和研究,在此一并表示感谢.
摘    要:对包头平原第四纪堆积物的年代地层、生物地层、岩石地层和磁性地层的研究表明,该区晚更新世—全新世地层可与我国华北晚更新世—全新世典型地层剖面——萨拉乌苏河滴哨沟湾剖面对比,并可进一步划分出萨拉乌苏组、城川组、大沟湾组和滴哨沟湾组。这一研究不仅重新厘定了包头平原这一时段地层的层序,完成大区域地层对比,同时也为研究包头地区乃至呼包盆地晚更新世—全新世古气候和古地理环境变迁提供了基础资料。

关 键 词:包头  第四纪地层  古环境变迁
文章编号:0253-4959(2007)02-0133-08
修稿时间:12 27 2006 12:00AM

SUBDIVISION AND CORRELATION OF THE LATE PLEISTOCENE-HOLOCENE STRATA IN THE BAOTOU AREA AND ITS PALEOENVIRONMENT VARIATION
DENG Jin-xian,LIU Zheng-hong,XU Zhong-yuan,YANG Zhen-sheng,WEN Quan-bo,LI Feng-jiang,SONG Hai-feng.SUBDIVISION AND CORRELATION OF THE LATE PLEISTOCENE-HOLOCENE STRATA IN THE BAOTOU AREA AND ITS PALEOENVIRONMENT VARIATION[J].Journal of Stratigraphy,2007,31(2):133-140.
Authors:DENG Jin-xian  LIU Zheng-hong  XU Zhong-yuan  YANG Zhen-sheng  WEN Quan-bo  LI Feng-jiang  SONG Hai-feng
Institution:College of Earth Science, Jilin University, Changchun, 130026
Abstract:Chronostratigraphic, biostratigraphic, lithostratigraphic, and magnetostratigraphic investigation of the Neogene sediments of the Baotou Plain suggests that the late Pleistocene—Holocene strata may be correlated with the Dishaogouwan profile at the Salawusu River, a Pleistocene—Holocene type section in North China. The strata can be further subdivided into the Salawusu Formation, Chengchuan Formation, Dagouwan Formation, and Dishaogouwan Formation. The study not only revises the Neogene stratigraphy in the Baotou Plain, which facilitates regional stratigraphic correlation, but also provides stratigraphic data for the study of Neogene paleoclimatic and paleogeographic changes in the Baotou area and the Hubao Basin.
Keywords:Baotou  Neogene strata  paleoenvironment change
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