CAJ | 학술논문

运用地震沉积学的理论，使用90°相位转换和地层切片等关键技术，结合钻测井资料，对滨南地区滨682井区古近纪沙河街组3个层序的砂体分布特征和沉积体系进行了精细研究。结果表明，该区东部和东南部浊积砂体较为发育。层序I早期浊积砂体分布面积较大，中期和晚期面积较小；层序Ⅱ早期和晚期浊积砂体分布范围较大，中期很小；层序Ⅲ主要分布在南部地区。证明该方法不但简单，而且减少了穿时问题，适合楔形沉积层序的分析研究。
운용지진침적학적이론，사용90°상위전환화지층절편등관건기술，결합찬측정자료，대빈남지구빈682정구고근기사하가조3개층서적사체분포특정화침적체계진행료정세연구。결과표명，해구동부화동남부탁적사체교위발육。층서I조기탁적사체분포면적교대，중기화만기면적교소；층서Ⅱ조기화만기탁적사체분포범위교대，중기흔소；층서Ⅲ주요분포재남부지구。증명해방법불단간단，이차감소료천시문제，괄합설형침적층서적분석연구。
By using the theory of seismic sedimentology, using 90 ° phase shift technology and formation slices technology, combining with drilling and logging wells datas, distribution characteristics of sand in three sequences and sedimentary system of No. 682 well in Binnan area in Paleogene Shahejie formation have been studied in detail. It is showed that turbidite sand bodies are well developed in eastern and southeastern area. The distribution square of turbidite sand bodies are large in early period of sequence I , while they are small in middle and later period; the distribution square of turbidite sand bodies are large in early and late period of sequence Ⅱ , while they are small in middle period; sequence Ⅲis mainly distributed in southern area. It is proved that the method is not only simple, but also can reduce the diachronous problem. It is suitable for carrying out analysis and study on wedge type sedimentary sequence.