Signal Estimation Technology Inc. Maher S. Maklad A Brief Overview of Optimal Seismic Resolution.

Slides:



Advertisements
Similar presentations
Signal Estimation Technology Inc. Maher S. Maklad Optimal Resolution of Noisy Seismic Data Resolve++
Advertisements

Seismic Resolution Lecture 8 * Layer Thickness top 20 ms base
Interpretational Applications of Spectral Decomposition
Signal Estimation Technology Inc. Maher S. Maklad A Brief Overview of Robust Multi-channel Seismic Inversion.
Professor Bill Mullarkey
Signal Estimation Technology Inc. Porosity or Sidelobes? An Application of Robust Multichannel Inversion Maher S. Maklad et al. Presented at the 1993 CSEG.
Reflection Seismic Processing
Multi-Component Seismic Data Processing
FilteringComputational Geophysics and Data Analysis 1 Filtering Geophysical Data: Be careful!  Filtering: basic concepts  Seismogram examples, high-low-bandpass.
Environmental and Exploration Geophysics II
Resident Physics Lectures
Introduction The aim the project is to analyse non real time EEG (Electroencephalogram) signal using different mathematical models in Matlab to predict.
GG450 April 22, 2008 Seismic Processing.
Predictive Deconvolution in Practice
Abrupt Feature Extraction via the Combination of Sparse Representations Wei Wang, Wenchao Chen, Jinghuai Gao, Jin Xu Institute of Wave & Information, Xi’an.
The recovery of seismic reflectivity in an attenuating medium Gary Margrave, Linping Dong, Peter Gibson, Jeff Grossman, Michael Lamoureux University of.
Establishing Well to Seismic Tie
Total Variation Imaging followed by spectral decomposition using continuous wavelet transform Partha Routh 1 and Satish Sinha 2, 1 Boise State University,
Image Enhancement.
Modeling of Mel Frequency Features for Non Stationary Noise I.AndrianakisP.R.White Signal Processing and Control Group Institute of Sound and Vibration.
Xi’an Jiaotong University 1 Quality Factor Inversion from Prestack CMP data using EPIF Matching Jing Zhao, Jinghuai Gao Institute of Wave and Information,
Beach Energy Ltd Haselgrove 3D Seismic Data Re-processing, 2014 Quash X – Crosspread Adaptive Linear Noise Attenuation Sept 3, 2014.
Formatting and Baseband Modulation
Seismic is not too complex for geologists - If you can understand convolution, you have it made. Simply stated, when downward traveling waves pass by a.
Geol 755: Basin Analysis Geophysics Week 1
McGraw-Hill©The McGraw-Hill Companies, Inc., 2004 Physical Layer PART II.
1-1 Basics of Data Transmission Our Objective is to understand …  Signals, bandwidth, data rate concepts  Transmission impairments  Channel capacity.
Lecture 1. References In no particular order Modern Digital and Analog Communication Systems, B. P. Lathi, 3 rd edition, 1998 Communication Systems Engineering,
Elastic Inversion Using Partial Stack Seismic Data: Case Histories in China.
Multisource Least-squares Reverse Time Migration Wei Dai.
Seismometry Seismology and the Earth’s Deep Interior Seismometer – The basic Principles u x x0x0 ugug umum xmxm x x0x0 xrxr uground displacement x r displacement.
Deconvolution Bryce Hutchinson Sumit Verma Objectives: -Understand the difference between exponential and surface consistent gain -Identify power line.
Transforms. 5*sin (2  4t) Amplitude = 5 Frequency = 4 Hz seconds A sine wave.
Ping Zhang, Zhen Li,Jianmin Zhou, Quan Chen, Bangsen Tian
Attribute- Assisted Seismic Processing and Interpretation 3D CONSTRAINED LEAST-SQUARES KIRCHHOFF PRESTACK TIME MIGRATION Alejandro.
SISMO Can we use the spectral ridges to estimate Q ? Marcílio Castro de Matos
Last week’s problems a) Mass excess = 1/2πG × Area under curve 1/2πG = × in kgs 2 m -3 Area under curve = -1.8 ×10-6 x 100 m 2 s -2 So Mass.
ReferencesInfo Elog Strata Geoview Fundamentals Open Seismic Wavelet Estimation Horizon Picks Low Frequency Model Inversion Near Offset Far Offset Open.
Authors: Sriram Ganapathy, Samuel Thomas, and Hynek Hermansky Temporal envelope compensation for robust phoneme recognition using modulation spectrum.
Statistical measures of instantaneous spectra Kui Zhang* and Kurt J. Marfurt 2008 AASPI Consortium annual meeting Not Gaussian!
Introduction to Deconvolution
Chapter 4: Baseband Pulse Transmission Digital Communication Systems 2012 R.Sokullu1/46 CHAPTER 4 BASEBAND PULSE TRANSMISSION.
Beach Energy Ltd Lake Tanganyika 2D Marine Seismic Survey Data Processing, 2014 Squelch Tests for Streamer Noise Attenuation Lines BST14B24 and BST14B67.
Impact of MD on AVO Inversion
The following discussions contain certain “forward-looking statements” as defined by the Private Securities Litigation Reform Act of 1995 including, without.
Seismic Imaging in GLOBE Claritas
SEISMIC INTERPRETATION
Environmental and Exploration Geophysics II
Electromagnetic Spectrum
EXPLORATION GEOPHYSICS. EARTH MODEL NORMAL-INCIDENCE REFLECTION AND TRANSMISSION COEFFICIENTS WHERE:  1 = DENSITY OF LAYER 1 V 1 = VELOCITY OF LAYER.
Overview of Stark Reality Plugins for OpendTect Coming soon to a workstation near you.
EEL 6586: AUTOMATIC SPEECH PROCESSING Speech Features Lecture Mark D. Skowronski Computational Neuro-Engineering Lab University of Florida February 27,
1 st semester 1436/  When a signal is transmitted over a communication channel, it is subjected to different types of impairments because of imperfect.
HIGH FREQUENCY GROUND MOTION SCALING IN THE YUNNAN REGION W. Winston Chan, Multimax, Inc., Largo, MD W. Winston Chan, Multimax, Inc., Largo, MD Robert.
Encoding How is information represented?. Way of looking at techniques Data Medium Digital Analog Digital Analog NRZ Manchester Differential Manchester.
Outline Transmitters (Chapters 3 and 4, Source Coding and Modulation) (week 1 and 2) Receivers (Chapter 5) (week 3 and 4) Received Signal Synchronization.
Data QC and filtering Bryce HutchinsonSumit Verma Objective: Consider the frequency range of different seismic features Look for low frequency and high.
WAVELET NOISE REMOVAL FROM BASEBAND DIGITAL SIGNALS IN BANDLIMITED CHANNELS Dr. Robert Barsanti SSST March 2010, University of Texas At Tyler.
1 Geophysical Methods Data Acquisition, Analysis, Processing, Modelling, Interpretation.
Does It Matter What Kind of Vibroseis Deconvolution is Used? Larry Mewhort* Husky Energy Mike Jones Schlumberger Sandor Bezdan Geo-X Systems.
The Frequency Domain Digital Image Processing – Chapter 8.
68th EAGE Conference and Exhibition, Vienna 1 Impact of Time Lapse Processing on 4D Simultaneous Inversion The Marlim Field Case Study C. Reiser * 1, E.
Speech Enhancement Summer 2009
Filtering Geophysical Data: Be careful!
New ProMAX modules for reflectivity calibration and noise attenuation
Accuracy of the internal multiple prediction when the angle constraints method is applied to the ISS internal multiple attenuation algorithm. Hichem Ayadi.
Wavelet estimation from towed-streamer pressure measurement and its application to free surface multiple attenuation Zhiqiang Guo (UH, PGS) Arthur Weglein.
Processing of the Field Data using Predictive Deconvolution
Presenter: Shih-Hsiang(士翔)
Combination of Feature and Channel Compensation (1/2)
Presentation transcript:

Signal Estimation Technology Inc. Maher S. Maklad A Brief Overview of Optimal Seismic Resolution

Signal Estimation Technology Inc. Seismic deconvolution aims at estimating a band-limited version of the earth’s reflectivity. This is achieved by compressing the time duration of the wavelet. In order to make the problem tractable, the reflectivity is commonly assumed to have a white spectrum; an assumption that has been invalidated by many researchers. A lot of research has aimed at compensating for the colour of the reflectivity, mainly using well log information. The presence of noise further complicates matters. Seismic noise not only make it difficult to visually detect primary reflections, but it is also amplified by wavelet compression filters, setting a limit on how far one can compress the seismic pulse. In practice, a noise attenuation technique such as FX prediction filtering or Radon filtering is called upon to address the noise problem. This adds more implicit assumptions about the constituents of seismic data. Resolve provides an algorithm for deconvolution of noisy data where the operator is designed based on the estimated signal-to-noise ratio spectra and the wavelet is estimated without white reflectivity assumption. The result is a more geologically faithful data set where the spectrum of the data follows the trend of the spectrum of well log reflectivity without using well logs. This is evidenced by the examples given in this presentation. Introduction

Signal Estimation Technology Inc. Wavelet Amplitude Spectra Estimated from the estimated signal not directly from the noisy data No white reflectivity assumption: spectrum of decon data follows the spectrum of well log reflectivity more closely, thus producing geologically more faithful data SNR  Used to estimate signal spectra  Used to shape the input wavelet spectrum leading to - improved resolution and - controlled noise amplification Required spectra o Estimated using a proprietary pole-zero modelling technique o Very accurate for short time windows - - operator focuses on the zone of interest - option for sliding time operator adapts to changes in spectra with time Unique Features of Resolve

Signal Estimation Technology Inc. Improved resolution with controlled noise amplification Better detection of geologic features: faults, channels, wedges, etc. A viable alternative to reprocessing old data Works well on scanned paper sections Geologically more faithful data  Improved horizon maps and attribute estimation  More accurate inversion  Improved reservoir characterization  More accurate reserve estimation and risk assessment Business Impact of Resolve

Signal Estimation Technology Inc. Your team is under constant pressure to extract the most information from corporate assets as accurately and swiftly as possible. This information provides the foundation on which your business makes decisions. These decisions are based on a perception of reality. The result of these decisions depends on the accuracy of the perception. How to use seismic attributes to enable more informed decisions for the identification, reduction and management of risk while maximizing reward? One answer is to investigate both standard and alternative interpretation workflows available to determine ways of validating and/or improving upon “current practices”. Resolution Optimization: Motivation

Signal Estimation Technology Inc. Anatomy of Seismic Data = Consists of several components : SEISMIC Seismic(t) = Wavelet(t) * Reflectivity(t) + noise(t) Convolutional Model Seismic attribute analysis uses information extracted from the seismic data or its constituents. Seismic Response Time Energy Source Wavelet * Earth Reflectivity + Noise

Signal Estimation Technology Inc. Earth Filter = Seismic Response Earth Reflectivity Noise + Time Noise Attenuation Observations: Signal-to-Noise Ratio (SNR) is often not stressed. * Consequences: Horizon time and amplitude maps as well as other seismic attributes leave something to be desired. For example see the impact of removing noise on the following horizon amplitude map.. GCWS_top Amplitude map Before After

Signal Estimation Technology Inc. Time. Energy Source = Seismic response Earth Reflectivity Noise + * Deconvolution attempts to undo the effect of the wavelet. The simple inverse wavelet operator will blow up the noise because the wavelet is band- limited with very high inverse at some frequencies. This prompted the need for sophisticated solutions. Convolutional Model Time Domain: Seismic(t) = Wavelet(t) * Reflectivity(t) + noise(t) Frequency Domain: Seismic(f) = Wavelet(f) x Reflectivity(f) + noise(f) Deconvolution of Noisy Data

Signal Estimation Technology Inc. Resolution Optimization Energy Source = Seismic response Earth Reflectivity Noise + Time * The objectives are : Improve resolution while controlling noise. To do this we need to: o Estimate the wavelet in the presence of noise o Shape the wavelet according to SNR.. Preserve the colour of the reflectivity. We should not impose the white reflectivity assumption. Well log generated Reflectivity Spectrum

Signal Estimation Technology Inc. Resolution Optimization ….results Before After

Signal Estimation Technology Inc. Before Resolve has made improvements in the following areas: Resolution Optimization ….validation Peak Frequency After Increased the bandwidth of the data from ~ 200 Hz to ~ 300 Hz. Increased peak frequency of the data from ~ 140 Hz to > 250 Hz. Made the spectrum of the data follow the spectrum of the log generated reflectivity more closely providing confidence in the spectral gains, and enhanced stratigraphic and structural interpretation. Bandwidth Before After Well log generated Reflectivity Spectrum

Signal Estimation Technology Inc. A Western Alberta Conglomerate Beach Play: Data Before Decon A series of beach Conglomerates, each capped by a coal sequence. The coals are closely spaced and strong reflectors.

Signal Estimation Technology Inc. A Western Alberta Conglomerate Beach Play: Data After Decon

Signal Estimation Technology Inc. A Western Alberta Conglomerate Beach Play: Power Spectra Before and After Decon in dB Before After Frequency in Hz

Signal Estimation Technology Inc. Deconvolution of Raw Stacks

Signal Estimation Technology Inc. Unfiltered, Unscaled Raw Stack

Signal Estimation Technology Inc. After PC-Filter

Signal Estimation Technology Inc. After PC-Filter and Resolve

Signal Estimation Technology Inc. Power Spectra Raw-StkPC-FilterResolve Frequency dB Down

Signal Estimation Technology Inc. Example 2: Raw Stack Shot Shot Trace Trace Tim e Figure 3-7 Time

Signal Estimation Technology Inc. After PC-Filter Figure 3-8 Tim e Shot Shot Trace Trace

Signal Estimation Technology Inc. Residuals = Raw – PC-Filtered Data Figure Time Shot Shot Trace Trace

Signal Estimation Technology Inc. Power & SNR Spectra of Raw and PC-Filtered Data WindowTWT (msec) A B C D E A B C D E Power SpectraRaw Stk Power SpectraPC-Filter SNR SpectraRaw Stk SNR SpectraPC-Filter Frequency Frequency Frequency Frequency dB Figure 3-10b

Signal Estimation Technology Inc. Figure 3-11 Tim e Shot Shot Trace Trace After PC-Filter and Resolve Time

Signal Estimation Technology Inc. Processor’s Final Stack Figure 3-12 Tim e Shot Shot Trace Trace Time

Signal Estimation Technology Inc Wavelet Spectra Cepstral Lag FFT Before After Crosspower Spectra Frequency Frequency Frequency Amplitude Post Resolve Analysis Amplitude Spectra from Wavelet Cepstrum dB Before After Figure 3-13

Signal Estimation Technology Inc. 8 Bit and Scanned Data

Signal Estimation Technology Inc. A Land Example : Input Data Time Shot Shot Trace Trace Zone of Interest

Signal Estimation Technology Inc. After Resolve Trace Trace Zone of Interest Stratigraphic trapStructural trap Time Shot Shot Trace Trace Time Shot Shot Trace Trace

Signal Estimation Technology Inc. After Before CEPSTRUM AMPLITUDE SPECTRUM FROM WAVELET WAVELET SPECTRA Amplitude dB Analysis Before and After Resolve Cepstral Lag Frequency (Hz) CROSSPOWER SPECTRA Frequency (Hz)

Signal Estimation Technology Inc. Original Processed Volume A Marine Example - Input Data

Signal Estimation Technology Inc. Original Processed Volume Spectrally Shaped Volume After Resolve

Signal Estimation Technology Inc. Note: Input data was 8bit filtered and scaled data from workstation Spectral displays Before and After Resolve Note: After post-stack spectral shaping the dominant frequency of the data has increased by ~ 40 Hz and the bandwidth has increased by ~20 Hz. Before After

Signal Estimation Technology Inc. Scanned Data Original

Signal Estimation Technology Inc. Scanned data after PC-Filter and Resolve After Noise Attenuation and Resolve

Signal Estimation Technology Inc. Spectral Shaping using Resolve™ Original Processed Volume

Signal Estimation Technology Inc. Spectrally Shaped Volume Spectral Shaping using Resolve™ Original Processed Volume

Signal Estimation Technology Inc. Impact of Resolve on Horizon Maps Here we have 3 versions of the same data Filtered pre-stack spectral whitened and FXY Decon Unfiltered Migrated Stack Resolve Applied to Unfiltered Migrated Stack A horizon map was extracted from each volume and displayed underneath the corresponding seismic. All maps show a channel. The extent of the channel is largest for the first version, smaller for the second and smallest for the Resolve version. The map generated from Resolve is more accurate due to the improved resolution (sharper events) and the geologically faithful image (no white reflectivity assumption used).

Signal Estimation Technology Inc. Filtered Pre-stack Spectral Whitened and FXY Decon

Signal Estimation Technology Inc. Unfiltered Migrated Stack

Signal Estimation Technology Inc. Unfiltered Migrated Stack After Resolve

Signal Estimation Technology Inc. Resolve improves the resolution of seismic data without amplification of noise (i.e. constrained by SNR). No white reflectivity assumption leading a better spectral representation of earth reflectivity. The attributes estimated after applying Resolve are noise- resistant and more geologically faithful for improved reservoir characterization. More accurate interpretation of horizons and faults. A viable alternative to reprocessing old data. Effective for scanned 8-bit data Conclusions.

Signal Estimation Technology Inc. Powerful Scientific Tools for all Phases of the Life Cycle of your Assets