维普中文期刊产品整合服务

Discovery of Late Cretaceous foraminifera in the Songliao Basin: Evidence from SK-1 and implications for identifying seawater incursions

查看全文 作  者:XI [1]DangPeng;WAN [1]XiaoQiao;FENG [2]ZhiQiang;LI [1]Shun;FENG [2]ZiHui;JIA [1]JianZhong;JING [1]Xia;SI [1]WeiMin 高影响力作者 机构地区:[1]School of Earth Science and Resources, China University of Geosciences (Beijing), Beijing 100083, China;[2]Exploration and Development Research Institute of Daqing Oil Field Company, Daqing 163712, China高影响力机构 出  处:《Chinese Science Bulletin》索引2011年第56卷第3期,共4页高影响力期刊 基  金:supported by the National Basic Research Program of China (2006CB-701403);the National Natural Science Foundation of China (40872016);the Graduate Innovative Research Fundation of China University of Geosciences (Beijing) 摘  要:The Songliao Basin is the largest oil-bearing basin in China.In the absence of sufficient evidence,the possibility of seawater incursion(s) into the Songliao Basin remains controversial.Recently,we discovered relatively abundant foraminifera fossils from units 1 and 2 of the Nenjiang Formation of borehole SK-1.Benthic foraminifera (Gavlinella sp.,Anomalinoides sp.,Pullenia sp.,Haplophragmoides sp.,Karrorulina hokkaidoana,Clavulinoides sp.),as well as planktonic foraminifera (Archaeoglobigerina blowi,Archaeoglobigerina cretacea and Hedbergella flandrini),were identified.These fossils were widely distributed in the marine Cretaceous.According to the global distribution of the above-mentioned planktonic foraminifera,the age of these fossil bearing strata appears to be Late Coniacian to Santonian.More importantly,these foraminifera provide direct evidence for marine water incursions into the Songliao Basin during deposition of the Lower Nenjiang Formation. 关 键 词:有孔虫化石 松辽盆地 海水入侵 晚白垩世 证据 水库 浮游有孔虫 底栖有孔虫
相关文献

参考文献(28)

引证文献(23)

网站首页 | 关于我们 | 联系我们 | 产品服务 | 客服中心 | 广告服务 | 版权声明 | 网站联盟 | 友情链接 | 售卡网点

版权所有© 渝B2-20050021-1 渝公网安备 50019002500403号 违法和不良信息举报中心

互联网出版许可证 新出网证(渝)字10号 全国400电话 - 免长途话费