黄清华,吴怀春,万晓樵,贺怀宇,邓成龙

• 1:大庆油田有限责任公司勘探开发研究院
• 2:中国地质大学地球科学与资源学院
• 3:中国科学院地质与地球物理研究所

摘要(Abstract)：

生物地层学研究表明,火石岭组、沙河子组和营城组均产Cicatricosisporites,Klukisporites,Densoisporites和Aequitriradites等早白垩世代表分子,登娄库组产Cicatricosisporites exilis-Hymenozonotriletes mesozoicus孢粉组合,它是中国北方Albian期的典型孢粉植物群,组合中的Kraeuselisporites majus,Scopusporis lautus,Bal mei-sporites holodictyus等多见于北美、澳大利亚等地同期地层中;泉头组产丰富的被子植物花粉化石,如Cranwelliastriatella,Xinjiangpollis minutus,Lythraidites debilis,Quantonenpollenites crassatus,Q.tari mensis,Scollardiatrapaformis,Beaupreaiditessp.,Gothanipollissp.等,这些被子植物花粉的出现,表明泉头组的地质时代不会早于Cenomanian期。锆石U-Pb年龄表明,火石岭组上部火山岩年龄为124.9±2.5 Ma,时代已上延至Barremian期;营城组火山岩、火山碎屑岩主峰年龄为105~112 Ma,其时代为晚Aptian—早Albian期,青山口组下部火山碎屑岩年龄为91.35±0.48 Ma,显示其时代已进入Turonian期,嫩江组二段下部火山碎屑岩年龄为83.68±0.47 Ma,显示其下限年龄为Santonian。磁性地层研究表明,泉头组四段至嫩江组一段为稳定的正极性,对应于白垩纪古海洋超静磁条带CNS上部;嫩江组二段至嫩江组五段为稳定的反极性带,它对应于白垩纪古海洋超静磁条带之后的第一个反极性带C33r;四方台组—明水组为混合极性带,它对应于白垩纪古海洋Campanian-Maastrichtian期混合极性带。

关键词(KeyWords)： 生物地层;年代地层;磁性地层;新进展;白垩系;松辽盆地

Abstract:

Keywords:

基金项目(Foundation): 国家重点基础研究发展计划“973”项目(2006CB701403);; 国家自然科学基金项目(No.40802012)资助成果

作者(Author): 黄清华,吴怀春,万晓樵,贺怀宇,邓成龙

DOI: 10.19839/j.cnki.dcxzz.2011.03.002

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