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Near-surface characterization and Vp/Vs analysis of a shale gas basin.

机译:页岩气盆地的近地表特征和Vp / Vs分析。

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摘要

The data from a multicomponent refraction survey acquired in Northeast British Columbia was used in this thesis to carry out P-wave and S-wave near-surface description and to undertake Vp/Vs analysis of shallow and deep formations. The datasets had good quality for picking first break arrivals and to process the reflection data successfully.;Three lines from the refraction survey were used for this study. An important feature was the confirmation of a channel that was detected through a previously acquired electromagnetic survey. The near-surface model obtained from P-wave data showed two layers with P-wave velocities of ∼ 1950 m/s for the first layer and ∼ 2800 m/s for the second layer. The SH-wave data from one of the lines showed three layers in the west end of the line and two layers to the east end of the line. The other line showed three layers along the entire profile. The S-wave velocity of the first layer was found to be around 375 m/s, that for the second layer was ∼ 727 m/s and the S-wave velocity for the third layer was --- 1400 m/s.;The velocity-depth structure obtained for the near-surface was used for the calculation of static corrections. As expected, S-wave static corrections gave higher values that the P-wave static corrections. The datum static corrections vary from -150 ms to -250 ms for SH-wave data and about -15 ms to 15 ms for P-wave data.;Vp/Vs analysis was performed for the near-surface structure with the values of velocities obtained from the refraction analysis and also through PP-PS registration for deeper structures. Measured values of Vp/Vs showed differences of around 0.1 when compared to those from well log. Values of Vp/Vs ranged from 5 in the near-surface to 2.2 in deeper formations.
机译:本文利用在不列颠哥伦比亚省东北部获得的多分量折射测量数据,对P波和S波进行近地表描述,并对浅层和深层地层进行Vp / Vs分析。该数据集具有良好的质量,可以很好地采集初次到达并成功处理反射数据。一个重要的功能是确认通过先前获得的电磁勘测检测到的通道。从P波数据获得的近地表模型显示出两层,第一层的波速为〜1950 m / s,第二层的波速为〜2800 m / s。来自其中一条线的SH波数据显示,在该线的西端为三层,而在该线的东端为两层。另一行显示整个轮廓上的三层。发现第一层的S波速度为约375m / s,第二层的S波速度为〜727m / s,第三层的S波速度为-1400m / s。从近表面获得的速度深度结构用于静态校正的计算。不出所料,S波静态校正比P波静态校正提供更高的值。 SH波数据的基准静态校正范围从-150 ms到-250 ms,P波数据的基准静态校正范围从-15 ms到15 ms .;对近地表结构进行了Vp / Vs分析,得到了速度值可以通过折射分析获得,也可以通过PP-PS配准获得更深的结构。与测井数据相比,Vp / Vs的测量值显示出约0.1的差异。 Vp / Vs的值范围从近地表的5到较深层的2.2。

著录项

  • 作者

    Zuleta Tobon, Liliana M.;

  • 作者单位

    University of Calgary (Canada).;

  • 授予单位 University of Calgary (Canada).;
  • 学科 Geophysics.
  • 学位 M.Sc.
  • 年度 2012
  • 页码 136 p.
  • 总页数 136
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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