Characteristics of Mudstone in Complex Fluvial Sedimentary System in Bohai L Oilfield

K. Huang, Chunsheng Shen, Kai Kang, Libing Wang, Zhongbo Xu, Lin Li
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Abstract

Bohai L oilfield develops a complex fluvial sedimentary system, which includes many types of fluvial sedimentary facies. Based on the coring well of oil field, the distribution characteristics of mudstone are analyzed, it is shown that the mudstone has similar internal structure and can be classified into four types according to its color: gray to grayish, variegated, brown to gray-brown and khaki, the assemblage has a large gray to grayish mudstone section, large gray to grayish mudstone intercalated thin layer sandstone, gray to grayish mudstone associated with variegated (brown) mudstone, grayish mudstone associated with lacustrine sand grain bedding sandstone, concomitant generation of large staggered bedding sandstone and grayish mudstone, mixed (gray-brown) mudstone associated with large staggered bedding sandstone, interaction between different colors of mudstone and sandstone and large interlaced sandstone intercalated with thin layer mudstone. The mudstone color is mainly gray and grayish, and very few oxidized mudstone is developed alone, which indicates that fluvial mudstone may be formed in the reductive environment in humid climate, and the fluvial mudstone in this area may be formed in the oxidizing environment, which is different from the general understanding of fluvial facies, the oxidation color is the result of the later transformation.
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渤海L油田复杂河流沉积体系泥岩特征
渤海L油田发育复杂的河流沉积体系,包括多种类型的河流沉积相。以油田取心井为基础,分析了泥岩的分布特征,认为泥岩内部结构相似,按颜色可分为4种类型:灰色到灰色、杂色、棕色到灰褐色和卡其色,组合中有大块灰色到灰色泥岩剖面,大块灰色到灰色泥岩夹层薄层砂岩,大块灰色到灰色泥岩伴生杂色(棕色)泥岩,大块灰色泥岩伴生湖相砂粒层理砂岩,大块交错层理砂岩和灰色泥岩伴生,大块交错层理砂岩伴生混合(灰褐色)泥岩,大块交错层理砂岩伴生混合(灰褐色)泥岩。不同颜色的泥岩与砂岩相互作用,大型夹层砂岩与薄层泥岩互插。泥岩颜色以灰色、灰白色为主,单独发育的氧化泥岩极少,说明河流泥岩可能形成于湿润气候下的还原环境,本区河流泥岩可能形成于氧化环境,这与一般对河流相的认识不同,氧化色是后期转化的结果。
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