西南石油大学学报(自然科学版) ›› 1994, Vol. 16 ›› Issue (3): 28-33.DOI: 10.3863/j.issn.1000-2634.1994.03.005

• 石油地质勘探 • 上一篇    下一篇

应用微地震相预测灰岩地层有利储渗带

朱仕军

  

  1. (石油勘探系)
  • 收稿日期:1993-12-24 修回日期:1900-01-01 出版日期:1994-08-20 发布日期:1994-08-20
  • 通讯作者: 朱仕军

Application of MicroseismicReserve-permeate Phases in Prediction of Favourable Belt in Limestone Layer

Zhu Shi-jun
  

  1. (Department of Geological Exploration)
  • Received:1993-12-24 Revised:1900-01-01 Online:1994-08-20 Published:1994-08-20
  • Contact: Zhu Shi-jun

摘要: 以沉积相、成岩作用研究为基础宏观评价选出的有利构造范围内,用徽地震相分析方法预侧
灰岩地层有利储渗带及裂缝发育带,再结合钻井、地质及测井解释结果,综合分析确定有利储渗带的特征与分布范圈.本文对川东福成寨构造、双家坝构造T53-1储层的徽地震相研究,预测结果表明,利用微地震相来预测灰岩地层有利储渗带的效果是很好的。

关键词: 徽地震相 地震波振幅 地震地层解释 储渗带 碳酸盐岩

Abstract: Based on the study of sedimentary facies and diagenesis,the characteristics and distribu-tion of favourable reserve-permeate belt in limestone layer can be determined through the analysis of microseismic phases of the belt as well as the interpretation of drilling,geology and logging. Through the discussion of the microseismic phases of Fu Cheng Zhai's and Shuang Jia Ba's T:-‘container constructions in the east of Sichuan Province,the paper tried to prove the effectiveness of the application of microseismic_ phases in the prediction of favourable reserve一permeate belt in limestone layer.

Key words: Microseismic phases Amplitude of seismic wave

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