Editorial office of ACTA PETROLEI SINICA ›› 2005, Vol. 26 ›› Issue (4): 58-62.DOI: 10.7623/syxb200504012

• Petroleum Exploration • Previous Articles     Next Articles

Coherency algorithm based on higher-order statistics and sedimentary evolvement analysis of sandstone bodies

YIN Cheng1, XIONG Xiao-jun2, ZHANG Bai-lin1, LIAO Xi-ming1, ZHOU Jie-ling1   

  1. 1. College of Resources and Environment, Southwest Petroleum Institute, Chengdu 610500, China;
    2. College of Information Engineering, Chengdu University of Technology, Chengdu 610059, China
  • Received:2004-07-16 Revised:2005-03-28 Online:2005-07-25 Published:2010-05-21

基于高阶统计量的相干体算法及砂体沉积演化分析

尹成1, 熊晓军2, 张白林1, 廖细明1, 周洁玲1   

  1. 1. 西南石油学院资源与环境学院 四川成都 610500;
    2. 成都理工大学信息工程学院 四川成都 610059
  • 作者简介:尹成,男,1965年6月生,1997年获成都理工学院工学博士学位,现为西南石油学院教授,主要从事高阶谱分析、非线性随机最优化方法和地震反演等研究.E-mail:yinnc2703@vip.163.com
  • 基金资助:
    国家高技术研究发展计划(863)项目(2003AA602110-5)资助.

Abstract: The higher-order statistics are insensitive to Gaussian noise and include more information than power spectrum.A new coherency algorithm based on higher-order statistics from the first generation of correlative coherency algorithm was presented.Fourth-order moment was used in the new algorithm,which makes the new algorithm has very fast calculating speed and strong valid for restraining Gaussian noise.The result of practical coherent time profiles indicates that the new algorithm can effectively enhance the continuity,which is helpful to track strata and explain faults.The evolving time slice figures of sedimentary environment can be obtained from the new algorithm.The new algorithm is useful for analyzing the sedimentary evolving process of sandstone bodies.

Key words: coherency body, higher-order statistics, fault interpretation, sedimentary environment, sandstone body evolvement

摘要: 高阶统计量比功率谱函数包含更多的信息,且对高斯噪声不敏感,为此以第一代基于相关的相干体算法为基础,提出了一种新的基于高阶统计量的相干体算法.该算法采用四阶矩函数进行计算,不仅计算速度快,而且抑制噪声能力强.实际资料的相干时间剖面表明,该算法有效地突出了地层的高连续性特征,有利于层位追踪和断层解释.利用该算法得到了沉积环境时间演化切片图,可将其应用于砂体的沉积演化分析.

关键词: 相干体, 高阶统计量, 断层解释, 沉积环境, 砂体演化

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