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双临界差异层间速度分析法的原理及应用
PRINCIPLE AND APPLICATION OF DOUBLE CRITICAL DIFFERENTIAL INTERFORMATION VELOCITY ANALYSIS
【摘要】 提出一种双临界差异层间速度分析法,其原理是利用纯泥岩、纯砂岩两种速度模型作为背景层速度,进行差异层间速度分析,进而预测地层岩性或含烃性。在吐哈盆地中侏罗统初步试验证明,双临界差异层间速度分析方法用于地层岩性预测有较高的精度。运用该分析方法指明了吐哈盆地胜北构造带储集体发育有利的部位。
【Abstract】 The principles of double critical differential interformation velocity analysis (DIVA)are studied. The technique of double critical DIVA is applied to study the middle Jurassic of Tuha basin. The result shows that the technique of double critical DIVA can be used to predict stratum lithologic with a high precision, and the good reservoirs in Shengbei structure zon of Tuha basin are proposed.
【关键词】 双临界DIVA;
地层岩性;
层速度;
吐哈盆地;
【Key words】 Double critical DIVA; Stratum Lithologic; Interformational velocity; Tuha basin;
【Key words】 Double critical DIVA; Stratum Lithologic; Interformational velocity; Tuha basin;
- 【文献出处】 石油大学学报(自然科学版) ,JOURNAL OF THE UNIVERSITY OF PETROLEUM,CHINA , 编辑部邮箱 ,1996年06期
- 【分类号】P618.13
- 【被引频次】1
- 【下载频次】80