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呼图壁地区双孔介质岩石物理建模与裂缝预测

钦黎明 程志国 郑伟 陈勇 苏艳丽 沈建文 宋建国

CT理论与应用研究2023,Vol.32Issue(6):723-734,12.
CT理论与应用研究2023,Vol.32Issue(6):723-734,12.DOI:10.15953/j.ctta.2023.117

呼图壁地区双孔介质岩石物理建模与裂缝预测

Rock Physics Modeling and Fracture Prediction of Double Porosity Media in the Hutubi Area

钦黎明 1程志国 1郑伟 1陈勇 1苏艳丽 1沈建文 2宋建国3

作者信息

  • 1. 中国石油新疆油田分公司勘探开发研究院地球物理所,乌鲁木齐 830013
  • 2. 赛哲尔能源科技(北京)有限公司,北京 100102
  • 3. 中国石油大学(华东)地球科学与技术学院,山东 青岛 266580
  • 折叠

摘要

Abstract

The deep target strata K1q,J3k and J2t in the Hutubi area have large-scale reservoirs and abundant oil and gas resources,but the traditional rock physics modeling of porous media cannot effectively distinguish oil and gas desserts from mudstones.Based on the systematic analysis of the logging curve characteristics of the target section,the shear wave velocity is corrected by the differential equivalent medium rock physics model,and the VPVSC and PIMP curves are restored by the Gassman equation fluid replacement,which highlights the sweet spot reservoir and mudstone discrimination.The linear sliding theory is introduced to establish the rock physics model of fractured reservoirs in dual-porosity media.The differential equivalent medium rock physics model for primary pores and the linear sliding model for anisotropic secondary fractures are organically integrated to realize the anisotropic medium rock physics modeling of the pore-fracture reservoir in the Hu 1-Hu 6 well area,and the rock physics plate is constructed.Combined with the anisotropic inversion of pre-stack OVT domain seismic data,the dominant reservoirs are effectively predicted.This paper has formed a complete set of deep fracture prediction method and technical processes,that provide a reference for the exploration and development of deep targets in similar exploration areas.

关键词

各向异性反演/双孔介质/岩石物理/裂缝预测

Key words

anisotropy inversion/dual-porous medium/rock-physical/fracture prediction

分类

天文与地球科学

引用本文复制引用

钦黎明,程志国,郑伟,陈勇,苏艳丽,沈建文,宋建国..呼图壁地区双孔介质岩石物理建模与裂缝预测[J].CT理论与应用研究,2023,32(6):723-734,12.

CT理论与应用研究

OACSTPCD

1004-4140

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