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STUDY ON SANDSTONE DISTRIBUTION AND SEDIMENTARY CHARACTERISTICS OFTHE FOURTH MEMBER OF SHAHEJIE FORMATION IN DAMINTUN SAG, CHINA

机译:巴德明顿凹陷沙河街组第四段砂岩分布及沉积特征研究

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B ased on geological exploration results and geophysical logging results, this paper studies the sandstone distribution and sedim entary system characteristics o f the Shahejie Form ation o f the D am intun sag oil and gas reservoir, and obtains the follow ing conclusions: the fourth section o f the Shahejie Form ation (Es4) in the study area The sand body o f the system dom ain is very developed, w ith the characteristics o f large sand body thickness and high sand content o f sand body, and its distribution has a good regularity in space. The sand body thickness o f the low -level system dom ain in the study area is 620 m eter, the m inim um value is 0m, and the average value is 64.15 m eter. T he sand body o f the Es4 lake expansion system in the fourth section o f the Shahejie Form ation in the study area is poorly developed. G enerally, the conglom erate o f the Shahejie Form ation in the study area is distributed from the northw est to the southeast. The m axim um thickness o f conglom erate is 247.5 m eter, the m inim um value is 0m , and the average value is 8.45 m eter. The high value area o f conglom erate thickness is m ainly located in the northw estern part o f the study area, and its thickness is generally greater than 60 m eter. T he sedim entary system types o f the fourth m em ber o f the Shahejie Form ation in the D am intun depression can be divided into three sedim entary system s: fan delta, lake and turbidite. B ased on the Sk-a, K g-a and C M plots o f the particle size param eters o f the sam ple, the partial deviation o f the E s4 reservoir is m ainly positively biased, reflecting that the sedim ent is w eakly m odified by the w ave; the sandstone o f the D am ingjie Form ation o f D am intun is poorly sorted.
机译:根据地质勘探结果和地球物理测井结果,本文研究了大溪凹陷油气藏沙河街组的砂岩分布和沉积体系特征,得出以下结论:研究区的沙河街组(Es4)该系统的砂体非常发达,具有砂体厚度大,砂体含沙量高的特点,其分布在空间上具有良好的规律性。研究区低层系统的砂体厚度为620 meter,最小值为0m,平均值为64.15 meter。研究区沙河街组第四段Es4湖扩张系统的砂体发育较差。通常,研究区沙河街组的砾岩分布从西北到东南。砾岩的最大厚度为247.5米,最小值为0m,平均值为8.45米。团块厚度的高值区域主要位于研究区域的北酯部分,其厚度通常大于60米。达姆河洼地第四系沙河街组的沉积体系类型可分为扇形,湖泊和浊积三种沉积体系。根据样品粒度参数的Sk-a,K ga和CM图可知,E s4储层的部分偏差主要是正偏的,反映出该沉积物已被一定程度的破坏。挥舞达明杰岩层的砂岩分类不善。

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