渤海菜州湾第四纪晚期以来微体化石组合特征和沉积环境演化

林防 王建中 李建芬 裴艳东 康慧. 渤海菜州湾第四纪晚期以来微体化石组合特征和沉积环境演化[J]. 地质通报, 2005, 24(9): 879-884.
引用本文: 林防 王建中 李建芬 裴艳东 康慧. 渤海菜州湾第四纪晚期以来微体化石组合特征和沉积环境演化[J]. 地质通报, 2005, 24(9): 879-884.
LIN Fang1,2,WANG Jianzhong1,LI Jianfen2,PEI Yandong2,KANG Hui2 1. Institute of Hydrogeology and Environmental Geology,CAGS,Shijiazhuang 050061,Hebei,China, 2. Tianjin Institute of Geology and Mineral Resources,China Geological Survey,Tianjin 300170,China. Characteristics of microfossil assemblages and evolution of the sedimentary environment since the late Quaternary in the Laizhou Bay, Bohai Sea[J]. Geological Bulletin of China, 2005, 24(9): 879-884.
Citation: LIN Fang1,2,WANG Jianzhong1,LI Jianfen2,PEI Yandong2,KANG Hui2 1. Institute of Hydrogeology and Environmental Geology,CAGS,Shijiazhuang 050061,Hebei,China, 2. Tianjin Institute of Geology and Mineral Resources,China Geological Survey,Tianjin 300170,China. Characteristics of microfossil assemblages and evolution of the sedimentary environment since the late Quaternary in the Laizhou Bay, Bohai Sea[J]. Geological Bulletin of China, 2005, 24(9): 879-884.

渤海菜州湾第四纪晚期以来微体化石组合特征和沉积环境演化

Characteristics of microfossil assemblages and evolution of the sedimentary environment since the late Quaternary in the Laizhou Bay, Bohai Sea

  • 对渤海莱州湾南岸央子镇YZ1钻孔取微体古生物样品18个,通过分析鉴定和地层对比,以及对微体古生物化石进行属种、丰度和分异度分析,共划分出4个化石组合层段.根据化石组合特征分析认为第Ⅰ、第Ⅱ微体化石组合为全新世海侵的产物.第Ⅰ组合代表了海进序列,沉积环境为潮上带-潮间带;第Ⅱ组合为海退序列,沉积环境为潮间带-潮下带.第Ⅲ、第Ⅳ组合分别是晚更新世2次海侵的产物.第Ⅲ组合为晚更新世末期海侵的产物,海侵规模较大,沉积环境为滨海潮坪-潮间带;第Ⅳ组合海侵规模较小,陆相因素增大,沉积环境为河口-滨岸带或者为海陆交互相.
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出版历程
修回日期:  2004-08-10
刊出日期:  2005-09-15

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