Geol 706 Geophysical Series & Filtering J. Louie 1st Meeting Wed. 1/21 9:30 LMR355 Schedule is Flexible
|
|
- Rosanna Snow
- 5 years ago
- Views:
Transcription
1 Filtering Dolby JPEG Compression Acoustic Imaging Tomography Seismic Imaging Spectra Downward Continuation East P Velocity, m/s West P r of i l e l t Elevation rp Graben Sca v e A c t i F a u nd o n Aba et ed D ach men t 20 m 20 m Scale Whitening Surround-Sound Phased Arrays Fourier Transform Sampling Theory Anti-Aliasing How do they DO that? find out in Geol 706 Geophysical Series & Filtering J. Louie louie@seismo.unr.edu 1st Meeting Wed. 1/21 9:30 LMR355 Schedule is Flexible Discrete Fourier Transform Z-plane and Spectra Filter Design Resolution & Variance Diffraction Imaging Paraxial Wave Equations Finite Differencing Phased Arrays
2 Buck Mesa R i n g c S y n l i n e Central Depression Buck Mesa #1 Well Section Section 2 Wyoming 420 UTAH Upheaval Dome Canyonlands Upheaval Dome Arizona N 2 km T 27 S T 28 S Murphy Range Unit #1
3 Buck Mesa Chinle Moenkopi Syncline Valley Central Depression Navajo Buck Mesa #1 Island in the Sky Kayenta Wingate Cutler Hermosa Salt Dome Paradox 1 km no vertical exaggeration Precambrian Mississippian Section 1 (oblique) Section 2 Buck Mesa Chinle Moenkopi Cutler Syncline Valley Central Depression Navajo Buck Mesa #1 Island in the Sky Kayenta Wingate Hermosa Paradox Pinched-Off Salt Diapir 1 km no vertical exaggeration Precambrian Mississippian Section 1 (oblique) Section 2 Original Crater Form Buck Mesa Chinle Moenkopi Cutler Syncline Valley Central Depression Impact Central Uplift Navajo Buck Mesa #1 Island in the Sky Kayenta Wingate Hermosa Relaxation of Crater Form? Paradox 1 km no vertical exaggeration Precambrian Mississippian Section 1 (oblique) Section 2
4 0 Raw Records 2Time, s s 2 0 f Filtered Records (a) (b)
5 0 Depth, km 1.5 Interpreted Section 1 0 W Distance, km 1.4 Artifacts Ring Syncline Axis E Depth, km Buck Mesa #1 Log Sonic Transit Time, µs/m Wingate Fm. Chinle Fm. Moenkopi Fm. Cutler Fm. Hermosa Fm. Top of Paradox Formation
6 0.0 A. Section of 30 s Noise Record from 200 m Array at Newhall Fire Station 20.0 Time, sec 30.0 Distance, m Frequency, Hz 24.9 B. Velocity-Spectral Analysis of Noise Array Slowness, sec/meter Vertical Particle Velocity after Hz BP Filter after Trace-Equalize E E-4 Spectral Ratio over Average Power at All Slownesses F-K Aliasing Rayleigh Phase Velocity, km/s 1.2 C. Noise Array Rayleigh Dispersion Interpreted Dispersion w/ Uncertainty Modeled Dispersion Fit D. Rosrine vs. Noise Array at Newhall F.S.? Surface Wave Period, sec Logged S Velocity Logged P Velocity Refraction P Velocity Noise Array S Model Extremal S Models Depth, m ? Velocity, km/s
7 Part I: Geophysical Time Series Analysis Introduction and Review Time Series Domains, Models Sampling, Z Transform Fourier Sums, Spectra Correlations Discrete Fourier Transform Nyquist, Comb Function Slow FT, Symmetries Fast FT, Doubling Lab 1 Z-transforms and spectra Quasi-Analytic Analyses The Z Plane Integration, Smoothing Causality, Oscillation Rational Filters, Instability Minimum Phase, Classification Lab 2 Spectra and the Z-plane Filter Design Hilbert Transform, Analytic Signal Instantaneous Attributes Spectral Factorization, Causality Butterworth Filters Phase and Group Delay Lab 3 Minimum phase Resolution and Variance Uncertainty Principles Expectation, Tradeoffs Crosscorrelation, Coherence Central Limit Theorem Lab 4 Resolution and noise Part II: Introduction to Seismic Imaging Introduction Background of seismic imaging Geophysical Exploration for Geothermal Resources:_ Advanced Seismic Technology Sept workshop presentation for the Geothermal Resources Council conference. PDFs of examples of imaging research to 2001 A national seismic imaging project - Earthscope and USArray What is Seismic Migration? Reproducibility of "noise" Simplifying assumptions Lab 5: Java applications Zero-Offset Methods Multiplicity and stacking Exploding reflector model Extrapolation and imaging Migration Impulse response and superposition Hand migration Dispersion relation for acoustic WE Downward continuation (image of 3-d examp.) 2-d Fourier transforms Phase-shift (Gazdag) migration F-K (Stolt) migration Lab 6: 2-d FFTs and migration Physical and geological factors Accuracy of seismic experiments Property variation and the acoustic WE Evanescent energy Paraxial wave equation Fourier derivation Planewave derivation Parabolic WE 15, 45, and 60 degree extrapolators Retarded coordinates Thin lens term, time & depth migrations Finite differencing Explicit methods Implicit methods Tridiagonal systems Stability Lab 7: Finite differencing Time-domain extrapolation Absorbing boundaries Perspective on extrapolation Lab 8: Monochrome wave extrapolation Dip filters Splitting and full separation 3-d migration Thin-lens term Lab 9: Time-domain downward continuation
8
9
10
Implicit 3-D depth migration by wavefield extrapolation with helical boundary conditions
Stanford Exploration Project, Report 97, July 8, 1998, pages 1 13 Implicit 3-D depth migration by wavefield extrapolation with helical boundary conditions James Rickett, Jon Claerbout, and Sergey Fomel
More informationOne-step extrapolation method for reverse time migration
GEOPHYSICS VOL. 74 NO. 4 JULY-AUGUST 2009; P. A29 A33 5 FIGS. 10.1190/1.3123476 One-step extrapolation method for reverse time migration Yu Zhang 1 and Guanquan Zhang 2 ABSTRACT We have proposed a new
More informationMandatory Assignment 2013 INF-GEO4310
Mandatory Assignment 2013 INF-GEO4310 Deadline for submission: 12-Nov-2013 e-mail the answers in one pdf file to vikashp@ifi.uio.no Part I: Multiple choice questions Multiple choice geometrical optics
More information1. A few words about EarthScope and USArray. 3. Tomography using noise and Aki s method
1. A few words about EarthScope and USArray 2. Surface-wave studies of the crust and mantle 3. Tomography using noise and Aki s method 4. Remarkable images of US crust (and basins)! Unlocking the Secrets
More informationstudies have suggested that impact could have formed the dome. To test the various hypotheses,
1 Submitted to Journal of Geophysical Research - Planets, 1999. Seismic reection study of Upheaval Dome, Canyonlands National Park, Utah Z. Kanbur, 1 J. N. Louie, 2 S. Chavez-Perez, 3 G. Plank, 4 and D.
More informationthat impact could have formed the dome. To test the various hypotheses, we
Seismic reection study of Upheaval Dome, Canyonlands National Park, Utah 1 Z. Kanbur, 1 J. N. Louie, 2 S. Chavez-Perez, 3 G. Plank, 4 and D. Morey 5;6 Abstract. The origin of Upheaval Dome, in Canyonlands
More informationA Petroleum Geologist's Guide to Seismic Reflection
A Petroleum Geologist's Guide to Seismic Reflection William Ashcroft WILEY-BLACKWELL A John Wiley & Sons, Ltd., Publication Contents Preface Acknowledgements xi xiii Part I Basic topics and 2D interpretation
More information1. How many unconformities exist in each column? Note that it is not the same number, necessarily, for each column!
Geology 103 Name(s): Lab 5: Sequence stratigraphy Introduction: In the previous lab, you were able to illustrate Walther s Law by showing how transgressive rock sequences mirrored the offshore facies sequence.
More informationPART A: Short-answer questions (50%; each worth 2%)
PART A: Short-answer questions (50%; each worth 2%) Your answers should be brief (just a few words) and may be written on these pages if you wish. Remember to hand these pages in with your other exam pages!
More informationSeismic reflection study of Upheaval Dome Canyonlands National Park Utah
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 105, NO. E4, PAGES 9489-9505, APRIL 25, 2000 Seismic reflection study of Upheaval Dome Canyonlands National Park Utah Z. Kanbur, 1 J. N. Louie, e S. Ch vez-p rez 3
More informationCalculation of the sun s acoustic impulse response by multidimensional
Calculation of the sun s acoustic impulse response by multidimensional spectral factorization J. E. Rickett and J. F. Claerbout Geophysics Department, Stanford University, Stanford, CA 94305, USA Abstract.
More informationSeismic Reflection Views of the 1994 Northridge Earthquake Hypocentral Region Using Aftershock Data and Imaging Techniques
Seismic Reflection Views of the 1994 Northridge Earthquake Hypocentral Region Using Aftershock Data and Imaging Techniques SERGIO CHÁVEZ-PÉREZ and JOHN N. LOUIE SEISMOLOGICAL LABORATORY/174, MACKAY SCHOOL
More informationElements of 3D Seismology Second Edition
Elements of 3D Seismology Second Edition Copyright c 1993-2003 All rights reserved Christopher L. Liner Department of Geosciences University of Tulsa August 14, 2003 For David and Samantha And to the memory
More information3. Lecture. Fourier Transformation Sampling
3. Lecture Fourier Transformation Sampling Some slides taken from Digital Image Processing: An Algorithmic Introduction using Java, Wilhelm Burger and Mark James Burge Separability ² The 2D DFT can be
More informationINTRODUCTION. The depth-variable-velocity prestack migration in offset-midpoint coordinates (Yilmaz, 1979) is formulated as
Stanford Exploration Project, Report 84, May 9, 2001, pages 1 58 Short Note Prestack migration by split-step DSR Alexander M. Popovici 1 INTRODUCTION The DSR prestack migration equation, though defined
More informationReflection Seismic Method
Reflection Seismic Method Data and Image sort orders; Seismic Impedance; -D field acquisition geometries; CMP binning and fold; Resolution, Stacking charts; Normal Moveout and correction for it; Stacking;
More informationFourier Analysis and Imaging Ronald Bracewell L.M. Terman Professor of Electrical Engineering Emeritus Stanford University Stanford, California
Fourier Analysis and Imaging Ronald Bracewell L.M. Terman Professor of Electrical Engineering Emeritus Stanford University Stanford, California 4u Springer Contents fa 1 PREFACE INTRODUCTION xiii 1 11
More informationP Wave Reflection and Refraction and SH Wave Refraction Data Processing in the Mooring, TN Area
P Wave Reflection and Refraction and SH Wave Refraction Data Processing in the Mooring, TN Area Abstract: Author: Duayne Rieger Home Institution: Slippery Rock University of Pennsylvania REU Institution:
More informationTOM 1.7. Sparse Norm Reflection Tomography for Handling Velocity Ambiguities
SEG/Houston 2005 Annual Meeting 2554 Yonadav Sudman, Paradigm and Dan Kosloff, Tel-Aviv University and Paradigm Summary Reflection seismology with the normal range of offsets encountered in seismic surveys
More informationTh Guided Waves - Inversion and Attenuation
Th-01-08 Guided Waves - Inversion and Attenuation D. Boiero* (WesternGeco), C. Strobbia (WesternGeco), L. Velasco (WesternGeco) & P. Vermeer (WesternGeco) SUMMARY Guided waves contain significant information
More informationSuggested directions for SEAM Pore Pressure Project
Suggested directions for SEAM Pore Pressure Project Dan Ebrom Classification: Internal Quantifying seismic velocity derived pore pressure prediction uncertainty Why? Pore pressure estimates from seismic
More informationSeismic Reflection Results: Stewart Gulch Region, Boise, Idaho
Seismic Reflection Results: Stewart Gulch Region, Boise, Idaho Report Prepared for The Terteling Company Boise, Idaho Lee M. Liberty Center for Geophysical Investigation of the Shallow Subsurface (CGISS)
More informationAnisotropic Seismic Imaging and Inversion for Subsurface Characterization at the Blue Mountain Geothermal Field in Nevada
PROCEEDINGS, 43rd Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, February 12-14, 2018 SGP-TR-213 Anisotropic Seismic Imaging and Inversion for Subsurface Characterization
More informationShort Note. Backprojection versus backpropagation in multidimensional linearized inversion. Cengiz Esmersoy* and Douglas Miller* - -
GEOPHYSICS. VOL. 54, NO. 7 (JULY 1989); P. 921-916, 3 FIGS. Short Note Backprojection versus backpropagation in multidimensional linearized inversion - - Cengiz Esmersoy* and Douglas Miller* INTRODUCTION
More informationPluto 1.5 2D ELASTIC MODEL FOR WAVEFIELD INVESTIGATIONS OF SUBSALT OBJECTIVES, DEEP WATER GULF OF MEXICO*
Pluto 1.5 2D ELASTIC MODEL FOR WAVEFIELD INVESTIGATIONS OF SUBSALT OBJECTIVES, DEEP WATER GULF OF MEXICO* *This paper has been submitted to the EAGE for presentation at the June 2001 EAGE meeting. SUMMARY
More informationNonstationary filters, pseudodifferential operators, and their inverses
Nonstationary filters, pseudodifferential operators, and their inverses Gary F. Margrave and Robert J. Ferguson ABSTRACT An inversion scheme for nonstationary filters is presented and explored. Nonstationary
More informationBME 50500: Image and Signal Processing in Biomedicine. Lecture 5: Correlation and Power-Spectrum CCNY
1 BME 50500: Image and Signal Processing in Biomedicine Lecture 5: Correlation and Power-Spectrum Lucas C. Parra Biomedical Engineering Department CCNY http://bme.ccny.cuny.edu/faculty/parra/teaching/signal-and-image/
More informationNew Evidence for Long-Term, Salt-Related Deformation at Upheaval Dome, SE Utah*
New Evidence for Long-Term, Salt-Related Deformation at Upheaval Dome, SE Utah* Patrick J. Geesaman 1, Bruce D. Trudgill 2, Thomas E. Hearon IV 3, and Mark G. Rowan 4 Search and Discovery Article #10756
More informationEstimation of Converted Waves Static Corrections Using CMP Cross- Correlation of Surface Waves
Static corrections using CCSW Estimation of Converted Waves Static Corrections Using CMP Cross- Correlation of Surface Waves Roohollah Askari, Robert J. Ferguson, J. Helen Isaac CREWES, Department of Geoscience,
More informationOn non-stationary convolution and inverse convolution
Stanford Exploration Project, Report 102, October 25, 1999, pages 1 137 On non-stationary convolution and inverse convolution James Rickett 1 keywords: helix, linear filtering, non-stationary deconvolution
More informationDirect Fourier migration for vertical velocity variations
V(z) f-k migration Direct Fourier migration for vertical velocity variations Gary F. Margrave ABSTRACT The Stolt f-k migration algorithm is a direct (i.e. non-recursive) Fourier-domain technique based
More informationSeismic tests at Southern Ute Nation coal fire site
Seismic tests at Southern Ute Nation coal fire site Sjoerd de Ridder and Seth S. Haines ABSTRACT We conducted a near surface seismic test at the Southern Ute Nation coal fire site near Durango, CO. The
More informationDR
DR2003071 0 0 270 0 30 0 90 0 60 0 120 0 150 0 90 0 180 0 180 0 A) RadialReceiverFunctions B ackazimuth (in degrees relative to north) -135-90 -45 0 45 90 135 180-5.0-2.5 Tangential R eceiver Functions
More informationStatic Corrections for Seismic Reflection Surveys
Static Corrections for Seismic Reflection Surveys MIKE COX Volume Editors: Series Editor: Eugene F. Scherrer Roland Chen Eugene F. Scherrer Society of Exploration Geophysicists Tulsa, Oklahoma Contents
More informationAPPENDIX A: Magnetotelluric Data in Relation to San Pedro Mesa Structural. The San Pedro Mesa structural high (discussed in main text of paper) was
Page of DR for GSA Special Paper 9, Chapter, Geophysical constraints APPENDIX A: Magnetotelluric Data in Relation to San Pedro Mesa Structural High The San Pedro Mesa structural high (discussed in main
More informationNonlinear acoustic imaging via reduced order model backprojection
Nonlinear acoustic imaging via reduced order model backprojection Alexander V. Mamonov 1, Vladimir Druskin 2, Andrew Thaler 3 and Mikhail Zaslavsky 2 1 University of Houston, 2 Schlumberger-Doll Research
More informationCompensating for attenuation by inverse Q filtering. Carlos A. Montaña Dr. Gary F. Margrave
Compensating for attenuation by inverse Q filtering Carlos A. Montaña Dr. Gary F. Margrave Motivation Assess and compare the different methods of applying inverse Q filter Use Q filter as a reference to
More informationSeismic Reflection Data and Conceptual Models for Geothermal Development in Nevada
Proceedings World Geothermal Congress 2010 Bali, Indonesia, 25-29 April 2010 Seismic Reflection Data and Conceptual Models for Geothermal Development in Nevada Glenn Melosh 1, William Cumming 2, John Casteel
More informationStanford Exploration Project, Report SERGEY, November 9, 2000, pages 683??
Stanford Exploration Project, Report SERGEY, November 9, 2000, pages 683?? 682 Stanford Exploration Project, Report SERGEY, November 9, 2000, pages 683?? Velocity continuation by spectral methods Sergey
More informationReversible Stolt migration
Reversible Stolt migration William A. Burnett Robert J. Ferguson ABSTRACT The nonstationary equivalent of the Fourier shift results in a general one-dimensional integral transform that applies to many
More informationIMAGING WITH REVERSE VERTICAL SEISMIC PROFILES USING A DOWNHOLE, HYDRAULIC, AXIAL VIBRATOR
IMAGING WITH REVERSE VERTICAL SEISMIC PROFILES USING A DOWNHOLE, HYDRAULIC, AXIAL VIBRATOR Mary Krasovec and Roger Turpening Earth Resources Laboratory Department of Earth, Atmospheric, and Planetary Sciences
More informationANGLE-DEPENDENT TOMOSTATICS. Abstract
ANGLE-DEPENDENT TOMOSTATICS Lindsay M. Mayer, Kansas Geological Survey, University of Kansas, Lawrence, KS Richard D. Miller, Kansas Geological Survey, University of Kansas, Lawrence, KS Julian Ivanov,
More information3D VISCO-ELASTIC WAVE PROPAGATION IN THE BORREGO VALLEY, CALIFORNIA
3D VISCO-ELASTIC WAVE PROPAGATION IN THE BORREGO VALLEY, CALIFORNIA Kim B OLSEN 1, Robert L NIGBOR 2 And Takaaki KONNO 3 SUMMARY We have simulated 2-Hz wave propagation in a three-dimensional model of
More informationComplex-beam Migration and Land Depth Tianfei Zhu CGGVeritas, Calgary, Alberta, Canada
Page 1 of 10 Home Articles Interviews Print Editions Complex-beam Migration and Land Depth Tianfei Zhu CGGVeritas, Calgary, Alberta, Canada DECEMBER 2012 FOCUS ARTICLE Summary Gaussian-beam depth migration
More informationAn Introduction to Geophysical Exploration
An Introduction to Geophysical Exploration Philip Kearey Department of Earth Sciences University of Bristol Michael Brooks Ty Newydd, City Near Cowbridge Vale of Glamorgan Ian Hill Department of Geology
More informationRefraction Microtremor for Shallow Shear Velocity in Urban Basins
Refraction Microtremor for Shallow Shear Velocity in Urban Basins John Louie, Nevada Seismological Lab UNR students: J. B. Scott, T. Rasmussen, W. Thelen, M. Clark Collaborators: S. Pullammanappallil &
More informationCENTER FOR INFRASTRUCTURE ENGINEERING STUDIES
1 CENTER FOR INFRASTRUCTURE ENGINEERING STUDIES Acquisition of an Engineering Seismograph By Dr. Neil Anderson UTC RE116 University Transportation Center Program at The University of Missouri-Rolla 2 Disclaimer
More informationA comparison of the imaging conditions and principles in depth migration algorithms
International Journal of Tomography & Statistics (IJTS), Fall 2006, Vol. 4, No. F06; Int. J. Tomogr. Stat.; 5-16 ISSN 0972-9976; Copyright 2006 by IJTS, ISDER A comparison of the imaging conditions and
More informationSUMMARY ANGLE DECOMPOSITION INTRODUCTION. A conventional cross-correlation imaging condition for wave-equation migration is (Claerbout, 1985)
Comparison of angle decomposition methods for wave-equation migration Natalya Patrikeeva and Paul Sava, Center for Wave Phenomena, Colorado School of Mines SUMMARY Angle domain common image gathers offer
More informationInvestigating fault shadows in a normally faulted geology
Investigating fault shadows in a normally faulted geology Sitamai Ajiduah* and Gary Margrave CREWES, University of Calgary, sajiduah@ucalgary.ca Summary Fault shadow poses a potential development risk
More information3. Magnetic Methods / 62
Contents Preface to the Second Edition / xv Excerpts from Preface to the FirstEdition / xvii Mathematical Conventions / xix 1. Introduction / 1 Reference / 5 2. Gravity Methods / 6 2. I. Introduction /
More informationObservation of shear-wave splitting from microseismicity induced by hydraulic fracturing: A non-vti story
Observation of shear-wave splitting from microseismicity induced by hydraulic fracturing: A non-vti story Petr Kolinsky 1, Leo Eisner 1, Vladimir Grechka 2, Dana Jurick 3, Peter Duncan 1 Summary Shear
More informationApplication of Seismic Reflection Surveys to Detect Massive Sulphide Deposits in Sediments-Hosted Environment
IOSR Journal of Applied Geology and Geophysics (IOSR-JAGG) e-issn: 2321 0990, p-issn: 2321 0982.Volume 3, Issue 4 Ver. I (Jul - Aug. 2015), PP 46-51 www.iosrjournals.org Application of Seismic Reflection
More informationIntroduction to the Mathematics of Medical Imaging
Introduction to the Mathematics of Medical Imaging Second Edition Charles L. Epstein University of Pennsylvania Philadelphia, Pennsylvania EiaJTL Society for Industrial and Applied Mathematics Philadelphia
More informationStolt residual migration for converted waves
Stanford Exploration Project, Report 11, September 18, 1, pages 1 6 Stolt residual migration for converted waves Daniel Rosales, Paul Sava, and Biondo Biondi 1 ABSTRACT P S velocity analysis is a new frontier
More informationLet us consider a typical Michelson interferometer, where a broadband source is used for illumination (Fig. 1a).
7.1. Low-Coherence Interferometry (LCI) Let us consider a typical Michelson interferometer, where a broadband source is used for illumination (Fig. 1a). The light is split by the beam splitter (BS) and
More informationV. Sajama, Bolivia. Kevin M. Ward, George Zandt, Susan L. Beck, Ryan C. Porter, Lara S. Wagner, Estela Minaya, Hernando Tavera
V. Sajama, Bolivia Kevin M. Ward, George Zandt, Susan L. Beck, Ryan C. Porter, Lara S. Wagner, Estela Minaya, Hernando Tavera Central Andean Plateau (CAP) Average elevation ~4 km Max width ~300 km Total
More informationEmpirical Green s Function Analysis of the Wells, Nevada, Earthquake Source
Nevada Bureau of Mines and Geology Special Publication 36 Empirical Green s Function Analysis of the Wells, Nevada, Earthquake Source by Mendoza, C. 1 and Hartzell S. 2 1 Centro de Geociencias, Universidad
More informationRock Physics and Quantitative Wavelet Estimation. for Seismic Interpretation: Tertiary North Sea. R.W.Simm 1, S.Xu 2 and R.E.
Rock Physics and Quantitative Wavelet Estimation for Seismic Interpretation: Tertiary North Sea R.W.Simm 1, S.Xu 2 and R.E.White 2 1. Enterprise Oil plc, Grand Buildings, Trafalgar Square, London WC2N
More informationTHE BETTER SUBSURFACE IMAGING USING A QUALITY SEISMIC PROCESSING
THE BETTER SUBSURFACE IMAGING USING A QUALITY SEISMIC PROCESSING Muchlis 1,Ibnu Rusydy 2, Marwan 3, Fakhrurrazi 3,Nurul Aflah 1,Asrillah 4 1 Departmen of Mining Engineering, Faculty of Engineering, University
More informationGEOL4714 Final Exam Fall 2005, C. H. Jones instructor
GEOL4714 Final Exam Fall 2005 p. 1 GEOL4714 Final Exam Fall 2005, C. H. Jones instructor Name: Student ID #: Feel free to use the back of the sheets for answers needing more space. (1) (10 pts) For each
More informationDHANALAKSHMI COLLEGE OF ENGINEERING DEPARTMENT OF ELECTRICAL AND ELECTRONICS ENGINEERING EC2314- DIGITAL SIGNAL PROCESSING UNIT I INTRODUCTION PART A
DHANALAKSHMI COLLEGE OF ENGINEERING DEPARTMENT OF ELECTRICAL AND ELECTRONICS ENGINEERING EC2314- DIGITAL SIGNAL PROCESSING UNIT I INTRODUCTION PART A Classification of systems : Continuous and Discrete
More informationPART 1. Review of DSP. f (t)e iωt dt. F(ω) = f (t) = 1 2π. F(ω)e iωt dω. f (t) F (ω) The Fourier Transform. Fourier Transform.
PART 1 Review of DSP Mauricio Sacchi University of Alberta, Edmonton, AB, Canada The Fourier Transform F() = f (t) = 1 2π f (t)e it dt F()e it d Fourier Transform Inverse Transform f (t) F () Part 1 Review
More informationIndex. p, lip, 78 8 function, 107 v, 7-8 w, 7-8 i,7-8 sine, 43 Bo,94-96
p, lip, 78 8 function, 107 v, 7-8 w, 7-8 i,7-8 sine, 43 Bo,94-96 B 1,94-96 M,94-96 B oro!' 94-96 BIro!' 94-96 I/r, 79 2D linear system, 56 2D FFT, 119 2D Fourier transform, 1, 12, 18,91 2D sinc, 107, 112
More informationDownloaded 05/01/17 to Redistribution subject to SEG license or copyright; see Terms of Use at
Mapping Imbricate Structures in the Thrust Belt of Southeast Turkey by Large-Offset Seismic Survey Oz Yilmaz*, Anatolian Geophysical, Istanbul, Turkey; and Serdar Uygun, Ali Ölmez, and Emel Çalı, Turkish
More informationNonlinear seismic imaging via reduced order model backprojection
Nonlinear seismic imaging via reduced order model backprojection Alexander V. Mamonov, Vladimir Druskin 2 and Mikhail Zaslavsky 2 University of Houston, 2 Schlumberger-Doll Research Center Mamonov, Druskin,
More informationSummary. We present the results of the near-surface characterization for a 3D survey in thrust belt area in Sharjah, United Arab Emirates.
Near-surface characterization, challenges, and solutions for high-density, high-productivity, Alexander Zarkhidze*, Claudio Strobbia, Abdallah Ibrahim, WesternGeco; Luis Viertel Herrera, Abdulla Al Qadi,
More informationSEG/New Orleans 2006 Annual Meeting. Non-orthogonal Riemannian wavefield extrapolation Jeff Shragge, Stanford University
Non-orthogonal Riemannian wavefield extrapolation Jeff Shragge, Stanford University SUMMARY Wavefield extrapolation is implemented in non-orthogonal Riemannian spaces. The key component is the development
More informationPlane-wave migration in tilted coordinates
Stanford Exploration Project, Report 124, April 4, 2006, pages 1 16 Plane-wave migration in tilted coordinates Guojian Shan and Biondo Biondi ABSTRACT Plane-wave migration in tilted coordinates is powerful
More informationPlane waves and spatial frequency. A plane wave
Plane waves and spatial frequency A plane wave Complex representation E(,) zt Ecos( tkz) E cos( tkz) o Ezt (,) Ee Ee j( tkz) j( tkz) o 1 cos(2 ) cos( ) 2 A B t Re atbt () () ABcos(2 t ) Complex representation
More informationSeismic attributes of time-vs. depth-migrated data using self-adaptive window
Seismic attributes of time-vs. depth-migrated data using self-adaptive window Tengfei Lin*, Bo Zhang, The University of Oklahoma; Zhifa Zhan, Zhonghong Wan, BGP., CNPC; Fangyu Li, Huailai Zhou and Kurt
More informationImproving the quality of Velocity Models and Seismic Images. Alice Chanvin-Laaouissi
Improving the quality of Velocity Models and Seismic Images Alice Chanvin-Laaouissi 2015, 2015, PARADIGM. PARADIGM. ALL RIGHTS ALL RIGHTS RESERVED. RESERVED. Velocity Volumes Challenges 1. Define sealed
More informationBy D.H. Lang 1 and J. Schwarz 1. This paper is an extract from
Identification of the Subsoil Profile Characteristics at the Coyote Creek Outdoor Classroom (CCOC), San José, from Microtremor Measurements - A Contribution to the CCOC Blind Comparison Experiment By D.H.
More informationIn The Shadow of a Headframe: Deep Exploration Using Integrated 3-D Seismic and BHEM Aat The Louvicourt Mine, Quebec
Geophysical Case Histories In The Shadow of a Headframe: Deep Exploration Using Integrated 3-D Seismic and BHEM Aat The Louvicourt Mine, Quebec 1. SEISServ, Quebec City, Quebec, Canada 2. Geoserve Logging
More informationImaging complex structure with crosswell seismic in Jianghan oil field
INTERPRETER S CORNER Coordinated by Rebecca B. Latimer Imaging complex structure with crosswell seismic in Jianghan oil field QICHENG DONG and BRUCE MARION, Z-Seis, Houston, Texas, U.S. JEFF MEYER, Fusion
More informationa) Piedmont: e) Monument: f) Plateau: g) Mesa: h) Butte: i) Playa: j) Perennial Stream:
Name: Lab day: Tuesday Wednesday CEEES/SC 10110L-20110L Planet Earth Laboratory Laboratory #11: Arid Environments & Landforms Readings: See handout at http://www.nd.edu/~cneal/physicalgeo/lab-deserts/index.html.
More informationJ.A. Haugen* (StatoilHydro ASA), J. Mispel (StatoilHydro ASA) & B. Arntsen (NTNU)
U008 Seismic Imaging Below "Dirty" Salt J.A. Haugen* (StatoilHydro ASA), J. Mispel (StatoilHydro ASA) & B. Arntsen (NTNU) SUMMARY Base and sub salt seismic imaging is still an unresolved issue. To solve
More informationApplication of High Resolution Seismic Survey in CBM Exploration A Case study, Sohagpur West Block, Madhya Pradesh
P - 421 Application of High Resolution Seismic Survey in CBM Exploration A Case study, Sohagpur West Block, Madhya Pradesh T. Seshunarayana, D.Viswaja*, K.N.S.S.S. Srinivas, P. Srinivasa Rao, S. Trupti,
More informationH Seismic imaging in and around salt bodies: problems and pitfalls. Ian Jones 1, Ian Davison 2. Summary
H1-2-3 Seismic imaging in and around salt bodies: problems and pitfalls Ian Jones 1, Ian Davison 2 1 ION, Chertsey, UK, 2 EarthMoves, Egham, UK Summary Salt movement often results in steeply-dipping complex
More informationAmplitude, Frequency and Bandwidth and their relationship to Seismic Resolution
Environmental and Exploration Geophysics II Amplitude, Frequency and Bandwidth and their relationship to Seismic Resolution tom.h.wilson wilson@geo.wvu.edu Department of Geology and Geography West Virginia
More informationESTIMATION FOR S-WAVE VELOCITY PROFILE USING RAYLEIGH WAVE INDUCED BY THE STANDARD PENETRATION TEST
4 th International Conference on Earthquake Geotechnical Engineering June 25-28, 2007 Paper No. 1395 ESTIMATION FOR S-WAVE VELOCITY PROFILE USING RAYLEIGH WAVE INDUCED BY THE STANDARD PENETRATION TEST
More informationOUTLINE. Many of us secretly dream of six months without gravity COURSE DESCRIPTION
GEOL 481.3 OUTLINE POTENTIAL FIELD METHODS GEOL 481.3 email: jim.merriam@usask.ca POTENTIAL FIELD METHODS Many of us secretly dream of six months without gravity Allan Fotheringham COURSE DESCRIPTION This
More informationA modeling and migration study of fault shadows: A synthetic example
Fault shadow imaging A modeling and migration study of fault shadows: A synthetic example Sitamai W. Ajiduah and Gary F. Margrave This report presents a study that uses 2D finite difference modeling and
More informationTh P7 02 A Method to Suppress Salt-related Converted Wave Using 3D Acoustic Modelling
Th P7 0 A Method to Suppress Salt-related Converted Wave Using 3D Acoustic Modelling J. Kumar* (Petroleum Geo-Services), M. Salem (ENI E&P), D.E. Cegani (ENI E&P) Summary Converted waves can be recorded
More informationA PML absorbing boundary condition for 2D viscoacoustic wave equation in time domain: modeling and imaging
A PML absorbing boundary condition for 2D viscoacoustic wave equation in time domain: modeling and imaging Ali Fathalian and Kris Innanen Department of Geoscience, University of Calgary Summary The constant-q
More informationSummary: Introduction:
Converted-wave processing of a 3D-3C refection seismic survey of Soda Lake geothermal field Tyler Kent* and John Louie, University of Nevada, Reno, Jim Echols, Magma Energy (U.S.) Corporation Summary:
More informationUnravel Faults on Seismic Migration Images Using Structure-Oriented, Fault-Preserving and Nonlinear Anisotropic Diffusion Filtering
PROCEEDINGS, 44th Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, February 11-13, 2019 SGP-TR-214 Unravel Faults on Seismic Migration Images Using Structure-Oriented,
More informationSEISMIC WAVE PROPAGATION. Lecture 2: Fourier Analysis
SEISMIC WAVE PROPAGATION Lecture 2: Fourier Analysis Fourier Series & Fourier Transforms Fourier Series Review of trigonometric identities Analysing the square wave Fourier Transform Transforms of some
More informationInterval anisotropic parameters estimation in a least squares sense Case histories from West Africa
P-263 Summary Interval anisotropic parameters estimation in a least squares sense Patrizia Cibin*, Maurizio Ferla Eni E&P Division (Milano, Italy), Emmanuel Spadavecchia - Politecnico di Milano (Milano,
More informationRegional Resource Area Mapping in Nevada Using the USArray Seismic Network
Regional Resource Area Mapping in Nevada Using the USArray Seismic Network Glenn Biasi, Ileana Tibuleac, and Leiph Preston Nevada Seismological Laboratory, University of Nevada Reno, Reno, NV 89557 Sandia
More informationCOMPLEX TRACE ANALYSIS OF SEISMIC SIGNAL BY HILBERT TRANSFORM
COMPLEX TRACE ANALYSIS OF SEISMIC SIGNAL BY HILBERT TRANSFORM Sunjay, Exploration Geophysics,BHU, Varanasi-221005,INDIA Sunjay.sunjay@gmail.com ABSTRACT Non-Stationary statistical Geophysical Seismic Signal
More informationG002 An Integrated Regional Framework for Seismic Depth Imaging in the Deepwater Gulf of Mexico
G002 An Integrated Regional Framework for Seismic Depth Imaging in the Deepwater Gulf of Mexico M. Davidson (Fugro Multi Client Services), M. Leander (Fugro Multi Client Services), K. Mohn (Fugro Multi
More informationPhase and group velocity measurements from physically modeled transmission gathers
Phase and group velocity measurements Phase and group velocity measurements from physically modeled transmission gathers Faranak Mahmoudian, Gary Margrave, and Joe Wong ABSTRACT Physical model data have
More informationEfficient outdoor sound propagation modelling in time-domain
Efficient outdoor sound propagation modelling in time-domain Timothy Van Renterghem Acoustics Group Department of Information Technology Ghent University/iMinds CEAS, X-Noise : Atm. and ground effects
More informationSEISMIC INVESTIGATION OF UNDERGROUND COAL FIRES; A FEASIBILITY STUDY AT THE SOUTHERN UTE NATION COAL FIRE SITE, DURANGO, COLORADO.
SEISMIC INVESTIGATION OF UNDERGROUND COAL FIRES; A FEASIBILITY STUDY AT THE SOUTHERN UTE NATION COAL FIRE SITE, DURANGO, COLORADO Sjoerd de Ridder, Department of Geophysics, Stanford University. Nigel
More informationThe seismic response to strong vertical velocity change
10 th Biennial International Conference & Exposition P-073 The seismic response to strong vertical velocity change Ian F. Jones, ION GX Technology Summary Conventional seismic data processing, whether
More informationMapping of complex geology in Banskandi and north plunge of Teidukhan areas of Assam using high resolution 2D seismic survey
10 th Biennial International Conference & Exposition P 002 Summary Mapping of complex geology in Banskandi and north plunge of Teidukhan areas of Assam using high resolution 2D seismic survey H.N.Garg*
More informationE : Lecture 1 Introduction
E85.2607: Lecture 1 Introduction 1 Administrivia 2 DSP review 3 Fun with Matlab E85.2607: Lecture 1 Introduction 2010-01-21 1 / 24 Course overview Advanced Digital Signal Theory Design, analysis, and implementation
More informationSubsalt imaging by common-azimuth migration
Stanford Exploration Project, Report 100, April 20, 1999, pages 113 125 Subsalt imaging by common-azimuth migration Biondo Biondi 1 keywords: migration, common-azimuth, wave-equation ABSTRACT The comparison
More informationSignal Modeling Techniques in Speech Recognition. Hassan A. Kingravi
Signal Modeling Techniques in Speech Recognition Hassan A. Kingravi Outline Introduction Spectral Shaping Spectral Analysis Parameter Transforms Statistical Modeling Discussion Conclusions 1: Introduction
More information