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VTI介质流体因子及各向异性参数直接反演方法

潘菲 李胜军 秦德文 陈康 高建虎 张广智

石油地球物理勘探2024,Vol.59Issue(4):875-886,12.
石油地球物理勘探2024,Vol.59Issue(4):875-886,12.DOI:10.13810/j.cnki.issn.1000-7210.2024.04.025

VTI介质流体因子及各向异性参数直接反演方法

Direct inversion method for fluid factors and anisotropy parameters in VTI media

潘菲 1李胜军 2秦德文 3陈康 4高建虎 2张广智1

作者信息

  • 1. 中国石油大学(华东)地球科学与技术学院,山东青岛 266580
  • 2. 中国石油勘探开发研究院西北分院,甘肃兰州 730020
  • 3. 中海石油(中国)有限公司上海分公司,上海 200335
  • 4. 中石油西南油气田公司勘探开发研究院,四川成都 610041
  • 折叠

摘要

Abstract

Reservoir fluid identification is an important research direction in the field of oil and gas exploration.Shale reservoirs have strong transverse isotropy with a vertical axis of symmetry(VTI),undeniably impacting fluid factor estimation.Based on the Rüger longitudinal wave reflection coefficient equation,this paper pro-poses an inversion method for fluid factor,Young's modulus,and anisotropy parameters based on the elastic impedance of VTI media.Firstly,a reflection coefficient approximate formula and an elastic impedance equa-tion represented by Russell fluid factor,Young's modulus,and equivalent anisotropic parameters are derived.Then,the fluid factor,Young's modulus,and anisotropic parameters are estimated through elastic impedance inversion,and the influence of anisotropic parameters on the inversion results is compared.Model testing and practical application of work area data show that this method can reasonably and accurately predict fluid factors,Young's modulus,and anisotropic parameters,providing a new method for identifying shale reservoir fluids,predicting brittle parameters,and predicting the anisotropic development degree.

关键词

储层/流体识别/等效各向异性/叠前反演/弹性阻抗

Key words

Reservoir/fluid identifying/equivalent anisotropy/prestack inversion/elastic impedance

分类

天文与地球科学

引用本文复制引用

潘菲,李胜军,秦德文,陈康,高建虎,张广智..VTI介质流体因子及各向异性参数直接反演方法[J].石油地球物理勘探,2024,59(4):875-886,12.

基金项目

本项研究受国家自然科学基金项目"高精度地震导向钻井关键技术及软件"(U23B6010)、"基于深度学习的深层裂缝储层参数地震反演方法"(42074136)和中国石油前瞻性基础性项目"复杂气藏地震识别与预测技术研究"(2021DJ0606)联合资助. (U23B6010)

石油地球物理勘探

OA北大核心CSTPCD

1000-7210

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