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哈密地区砂岩地震波速的实验研究

王怀民 王红才 殷昌吉 张翔宇 李阿伟 杜威

物探化探计算技术2017,Vol.39Issue(4):533-542,10.
物探化探计算技术2017,Vol.39Issue(4):533-542,10.DOI:10.3969/j.issn.1001-1749.2017.04.14

哈密地区砂岩地震波速的实验研究

The experiments on seismic velocity of sandstones in Hami

王怀民 1王红才 2殷昌吉 2张翔宇 3李阿伟 1杜威2

作者信息

  • 1. 中国石油大学(北京),地球科学学院,北京 102249
  • 2. 中国地质科学院地质力学研究所,北京 100081
  • 3. 中石化新星湖北新能源开发有限公司,武汉430000
  • 折叠

摘要

Abstract

Seismic velocity of rocks have a wide range of applications in regional tectonic research and shallow seismic exploration.Hami region is one of the important production bases for oil and gas in China,but there is no data of seismic velocity.Deep environment is simulated in laboratory and the change rule of P-and S-wave velocity which come from four groups of sandstones in Hami is studied in this paper.The result shows that the P-wave and S-wave velocity increase (or decrease) with the pressure at the logarithmic rule.The porosity of sandstone affect the rate and size of increased wave velocity.The lag effect of sandstone's wave velocity mainly in the procession that wave velocity of decompression is greater than boost when they are under the same pressure.The wave velocity with high pressure is closed to the theoretical wave velocity of space averaging models.Wave velocity data measured by experiment is consistent with the log data in Hami.Therefore it can be used as the auxiliary condition to define oil layer,water layer and dry layer.

关键词

哈密地区/砂岩/压力/地震波速/测井

Key words

Hami region/sandstone/pressure/seismic velocity/well logging

分类

天文与地球科学

引用本文复制引用

王怀民,王红才,殷昌吉,张翔宇,李阿伟,杜威..哈密地区砂岩地震波速的实验研究[J].物探化探计算技术,2017,39(4):533-542,10.

基金项目

中国地质调查局项目(DD20160060) (DD20160060)

物探化探计算技术

OACSCDCSTPCD

1001-1749

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