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REE Characteristics and Its Geological Significance of the Permo-Carboniferous in Bohaiwan Basin
Author(s): 
Pages: 589-596
Year: Issue:  4
Journal: ACTA SEDIMENTOLOGICA SINICA

Keyword:  稀土元素石炭-二叠系古环境物源渤海湾盆地;
Abstract: 采集了渤海湾盆地周缘露头剖面和盆内钻井岩心的泥岩及少量灰岩样品,采用电感耦合等离子质谱技术对样品进行了系统的稀土元素测试分析.测试样品稀土总量平均值为290.39 μg/g,明显大于北美页岩组合样.各样品δEu为0.42~0.83,平均0.67,中度Eu负异常;大多样品Ce含量正常,δCe为0.51~1.22,平均0.97.稀土元素配分模式总体为轻稀土富集、重稀土亏损型,轻稀土段曲线明显"右倾",重稀土段则较为"平坦".灰岩及部分泥岩中Ce的负异常指示了晚石炭世本区陆表海的沉积环境特点,古海水为氧化环境.根据稀土元素的Eu异常及总的元素组合特点,判断渤海湾盆地石炭-二叠系沉积物主要来自盆地北缘的阴山古陆,母岩类型为花岗岩.
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