西藏定日贡扎上白垩统的年代地层划分及评述  

Chronostratigraphic division and remarks of the Upper Cretaceous from Gongza of Dingri,Tibet,China

作　　者：石和[1] 黄思静[1] 李祥辉[1] 罗威[1] 常晓琳[1] 

机构地区：[1]成都理工大学沉积地质研究院,成都610059

出　　处：《成都理工大学学报（自然科学版）》2008年第2期181-186,共6页Journal of Chengdu University of Technology: Science & Technology Edition

基　　金：国家自然科学基金资助项目(4067207240272059)

摘　　要：分别采用不同的地层学方法对西藏贡扎地区的两条相邻上白垩统剖面进行了年代地层划分。根据将建立在贡扎Ⅰ上白垩统剖面上的锶同位素演化曲线与W.H.Burke等的同时代锶同位素演化曲线对比,剖面上岗巴村口组顶界年龄值约为81.4 Ma;根据在贡扎Ⅱ剖面上划分出的12个浮游有孔虫化石带确定的岗巴村口组顶界年龄值约为67.0 Ma。作者认为岗巴村口组顶界年龄值存在明显差别是受诸多因素影响,在对地层进行年代地层研究中,要不断提高各种地层学方法的分辨率,并尽可能采用综合的地层学方法。Two sections of Upper Cretaceous have been chronostratigraphically divided separately by different stratigraphic methods in Gongza of Gangba, Dingri, Tibet. The age of the top boundary of the Gangbacunkou Formation in Section Ⅰ is about 81.4 Ma based on the correlation between the Srisotopic curve set up in this section and the coeval curve set up by W. H. Burke et al（1982） in Western Interior USA. The age of this boundary in Section Ⅱ is about 67. 0 Ma based on 12 planketic foraminifera fossil zones. This paper points out that the obviious difference of the age of the top boundary of the Gangbacunkou Formation in the two adjacent sections was brought by several factors, and that the resolution of stratigraphical methods should be iraproved and a comprehensive method should be adopted in chronostrtigraphic division.

关 键 词：浮游有孔虫生物地层学 锶同位素地层学 年代地层划分 上白垩统 西藏贡扎 

分 类 号：P534.53[天文地球—古生物学与地层学]