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沉积岩的速度、衰减与岩石物理性质间的关系
引用本文:安勇,牟永光,方朝亮.沉积岩的速度、衰减与岩石物理性质间的关系[J].石油地球物理勘探,2006,41(2):188-192.
作者姓名:安勇  牟永光  方朝亮
作者单位:中科院地质与地球物理研究所,中国石油大学,CNPC科技发展部 北京市昌平区中国石油大学资源与信息学院102249,北京
摘    要:本文用Toksoz等人提出的频谱振幅法对砂、泥岩样品的纵、横波速度(vP、vS)及其品质因子(QP、QS)进行了实验室测试,得到以下结论:对于干燥岩石,衰减与频率无关,且纵、横波速度之间存在着强相关性;纵波速度和纵波品质因子呈弱相关性,横波速度与横波品质因子呈强相关性;纵波品质因子与横波品质因子呈强相关性;孔隙率与纵、横波速度有线性关系;岩石的衰减受岩性的影响,泥岩的衰减大干砂岩的衰减,含砾砂岩衰减大干不含砾砂岩。

关 键 词:岩石物理性质  频谱振幅法  速度  衰减  品质因子  纵波  横波
收稿时间:2005-06-24
修稿时间:2005-06-24

Relationship between attenuation, velocity of sedimentary rocks and petrophysical property.
An Yong,Mu Yong-guang and Fang Chao-liang. College of Resource and Information,China University of Petroleum,Changping District,Beijing City,China.Relationship between attenuation, velocity of sedimentary rocks and petrophysical property.[J].Oil Geophysical Prospecting,2006,41(2):188-192.
Authors:An Yong  Mu Yong-guang and Fang Chao-liang College of Resource and Information  China University of Petroleum  Changping District  Beijing City    China
Affiliation:An Yong,Mu Yong-guang and Fang Chao-liang. College of Resource and Information,China University of Petroleum,Changping District,Beijing City,102249,China
Abstract:The paper uses frequency-amplitude ratio method presented by Mr. Toksoz et al for laboratory test of velocities (VP, VS) and quality factors (QP, QS) of P- and S-waves in sandstone and mud-stone samples and obtained following conclusions: the attenuation is irrelative to frequency and there is strong correlation between P-wave velocity and S-wave velocity for dry rocks ; the P-wave velocity is weak correlative to P-wave quality factor and S-wave velocity is strong correlative to S-wave quality factor; P-wave quality factor is strong correlative to S-wave quality factor; porosity is linear with P- and S-waves velocities; the attenuation of rocks comes under the influence of lithology, the attenuation of mudstone is greater than that of sandstone and gravel-packing sand is greater than that without gravel pack.
Keywords:petrophysical property  frequency-amplitude ratio method  velocity  attenuation  quality factor  P-wave  S-wave
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