The Wave Equation Modeled

Slides:



Advertisements
Similar presentations
Tom Wilson, Department of Geology and Geography Environmental and Exploration Geophysics II tom.h.wilson Department of Geology.
Advertisements

Tom Wilson, Department of Geology and Geography Environmental and Exploration Geophysics II tom.h.wilson Department of Geology.
8. Ocean Crustal Structure and Seismic Reflection William Wilcock (via Michelle W.) OCEAN/ESS 410.
Seismic Reflection Ground Roll Filtering Ted Bertrand SAGE 2004.
GG450 April 22, 2008 Seismic Processing.
What is a reflector? There are many reflectors on a seismic section. Major changes in properties usually produce strong, continuous reflectors as shown.
I. Basic Techniques in Structural Geology
Seismic refraction and reflection projects and the traditional field camp Bob Bauer and Eric Sandvol University of Missouri Branson Field Lab.
الانعكاس السيزمي Receivers source reflector.
Lab 2 Seismogram Interpretation
Fundamentals Introduction Seismic waves: Propagation Velocity and Amplitudes Seismogram Measurement systems Sources, receivers, Acquisition strategies.
Occurs when wave encounters sharp discontinuities in the medium important in defining faults generally considered as noise in seismic sections seismic.
Reflection Field Methods
Filters  Temporal Fourier (t f) transformation  Spatial Fourier (x k x ) transformation applications  f-k x transformation  Radon (-p x ) transformation.
Waves: Phase and group velocities of a wave packet
Land and Marine Seismic Acquisition from 2D to 3D
Tom Wilson, Department of Geology and Geography Environmental and Exploration Geophysics II tom.h.wilson Department of Geology.
Seismic reflection Ali K. Abdel-Fattah Geology Dept.,
Geology 5660/6660 Applied Geophysics 26 Feb 2014 © A.R. Lowry 2014 For Fri 28 Feb: Burger (§8.4–8.5) Last Time: Industry Seismic Interpretation.
Geology 5660/6660 Applied Geophysics 18 Feb 2014 © A.R. Lowry 2014 For Wed 20 Feb: Burger (§ ) Last Time: Reflection Data Processing Step.
Processing Lab 9 Objectives: - View a timeslice - Consider binning effects on migration - Post stack Migration Sumit VermaBryce Hutchinson.
5. Seismology William Wilcock OCEAN/ESS 410. A. Earthquake Seismology.
Tom Wilson, Department of Geology and Geography Environmental and Exploration Geophysics II tom.h.wilson Department of Geology.
Geology 5660/6660 Applied Geophysics 28 Feb 2014 © A.R. Lowry 2014 Last Time: Ground Penetrating Radar (GPR) Radar = electromagnetic radiation (light)
Tom Wilson, Department of Geology and Geography Environmental and Exploration Geophysics II tom.h.wilson Department of Geology.
GravStat™ A OEX Technology Registered in the U. S. Patent and Trademark Office and offered through Lockhart Geophysical GravStat™ A method of determining.
Tom Wilson, Department of Geology and Geography Environmental and Exploration Geophysics II tom.h.wilson Department of Geology.
Introduction to Seismology
Data QC and filtering Bryce HutchinsonSumit Verma Objective: Consider the frequency range of different seismic features Look for low frequency and high.
Reflection seismograms
Geology 5660/6660 Applied Geophysics Last time: The Refraction Method Cont’d Multiple Horizontal Layers: Using Snell’s law, generalizes simply to: Dipping.
1 Geophysical Methods Data Acquisition, Analysis, Processing, Modelling, Interpretation.
Geology 5660/6660 Applied Geophysics 29 Feb 2016 © A.R. Lowry 2016 Last Time: Ground Penetrating Radar (GPR) Radar = electromagnetic radiation (light)
Geology 5660/6660 Applied Geophysics 12 Feb 2016
Geology 5660/6660 Applied Geophysics 26 Feb 2016 © A.R. Lowry 2016 For Mon 29 Feb: Burger (§8.4) Last Time: Industry Seismic Interpretation Seismic.
Microtremor method Saibi. Dec, 18, 2014.
Lee M. Liberty Research Professor Boise State University.
I. Basic Techniques in Structural Geology Field measurements and mapping Terminology on folds and folds Stereographic projections From maps to cross-sections.
Geology 490M 3D Seismic Workshop tom.h.wilson Department of Geology and Geography West Virginia University Morgantown, WV Demo, Wave.
Geology 5660/6660 Applied Geophysics 5 Feb 2016
Seismic Refraction Interpretation
Fang Liu and Arthur Weglein Houston, Texas May 12th, 2006
I. Basic Techniques in Structural Geology
Geology 5660/6660 Applied Geophysics 15 Mar 2016 Lab 5 GPR
Single fold vs. Multi-fold CMP seismic profiling
Introduction to Seismology
Reflection velocity analysis
Reflection Seismic Method
Applied Geophysics Fall 2016 Umass Lowell
Introduction to Seismology
Creating a Conference Poster
Environmental and Exploration Geophysics II
Marine Reflection Seismology - Geometry
Exploration and Environmental Geophysics
Acoustic Reflection 2 (distance) = (velocity) (time) *
The radar band is loosely taken to extend from approximately 0
Wave-Equation Migration Research at Los Alamos National Laboratory
Objectives of Well-Seismic Ties
From Raw Data to an Image
Seismic-Well Tie Flow-Chart
Figure 1 (from Fowler p 120 The configuration for the 110N 36 channel active source refraction survey: Long survey: Source is at x=0, geophone #1 is.
Prestack Depth Migration in a Viscoacoustic Medium
Geophysics/Tectonics
3D Seismic Processing Eric Verschuur AES 1530.
Waves: Phase and group velocities of a wave packet
—Based on 2018 Field School Seismic Data
WAVES.
Reflected, Refracted and Diffracted waves
Normal Incidence (coincident source-receiver) Ray-Tracing
Presentation transcript:

The Wave Equation Modeled We’ve looked at what happens to P-waves in the simple two-layer case...

The Wave Equation Modeled …we get a direct P-wave, a refracted P-wave, and a reflected P-wave.

The Wave Equation Modeled So, you can now easily find the three P-wave phases:

The Wave Equation Modeled …but, as you saw in your lab field data, real data adds the complication of other phases–here, the air wave and ground roll (Rayleigh wave) are shown.

Multilayer Model Remember, for refraction data you generally only need to know the first arrivals… Distance Direct Wave 1st Layer Refraction Time 2nd Refraction

Reflection/Refraction Refraction Advantages: Small number of sources/receivers can work Little signal processing is needed Interpretation straight forward Reflection Advantages: Small scale features can be resolved No restriction on velocity-depth profile Can be used in regions of complex geology Uses entire reflected wavefield Subsurface directly imaged

Seismic Reflection Terms: Stacked Section/Seismic Section: A plot of seismic reflection data with substantial digital processing that represents a zero-offset profile. Time Section: A seismic section in which the axes are offset and two-way travel time. Rarely represent correct spatial positioning of subsurface features. Depth Section: A seismic section in which the time section has been converted to depth through a velocity model.

Seismic Reflection Data Processing Steps Unlike refraction data, there are many processing steps to create an image of the subsurface with seismic reflection data. Many of these are not trivial, and we will look at some of them in lab. Poorly processed seismic data can be made to look like just about anything. You’ve been warned!

Seismic Reflection Data The basis of common midpoint (CMP) processing is to create a stacked profile representing a zero-offset section. CMP processing is the current industry standard.

Seismic Reflection Data

Seismic Reflection Data

Seismic Reflection Data Processing Problems… Best Data Poorly Processed Data

Seismic Reflection Data Examining Raw Data...

Seismic Reflection Data Examining Raw Data… Be aware that seismic data is as varied as geologic settings, and thus can look very different.

Seismic Reflection Data Digital filtering is a critical processing step...

Seismic Reflection Data You data can be analyzed in other domains as well as the frequency domain.