摘要
研究表明,兴I组砂岩只在工区东部发育,发育范围小;兴Ⅱ组砂岩发育范围大,全区发育,叠加厚度大;兴Ⅲ组砂岩大面积连片分布,大于15m的区域在井区西部,东南部局部相变为泥岩;兴Ⅳ组砂体以中部最厚,向东西两侧逐渐减薄。
The study shows that the sandstone of Xing I formation only develops in the east of the work area, and its development range is small. And the sandstone of XingⅡ formation has a large development range, developed in the whole area and has a large superimposed thickness. The sandstone of Xing Ⅲ formation is distributed in large contiguous areas, the area larger than 15 m is in the west of the well area, and the local facies in the southeast turn into mudstone. The sand body of Xing Ⅳ formation is the thickest in the middle, and it gradually thins towards the east and west sides.
引文
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