Purposes for Well-Seismic Ties & Quality

Slides:



Advertisements
Similar presentations
Well-Seismic Ties Lecture 7 Depth Time Synthetic Trace SLIDE 1
Advertisements

Seismic Reflections Lecture Shot Receiver Seismic Record
Wedge Modeling HRS-9 Hampson-Russell Software
Seismic Stratigraphy EPS 444
Signal Estimation Technology Inc. Porosity or Sidelobes? An Application of Robust Multichannel Inversion Maher S. Maklad et al. Presented at the 1993 CSEG.
Course 7: utilities and integration. Digitize log program.
Multicomponent seismic interpretation of the Marcellus shale
Isopach and Isochore Maps
Environmental and Exploration Geophysics II tom.h.wilson Department of Geology and Geography West Virginia University Morgantown, WV.
Wavelet Extraction using Seismic Interferometry C. Boonyasiriwat and S. Dong November 15, 2007.
November 19, 2001 Seismic modelling of coal bed methane strata, Willow Creek, Alberta Sarah E. Richardson, Rudi Meyer, Don C. Lawton, Willem Langenberg*
An array analysis of seismic surface waves
Environmental and Exploration Geophysics II tom.h.wilson Department of Geology and Geography West Virginia University Morgantown, WV.
Uncertainty in AVO: How can we measure it? Dan Hampson, Brian Russell
Overview of Stark Reality Plugins for OpendTect Coming soon to a workstation near you.
Joel Ben-Awuah. Questions to Answer What do you understand about pseudo-well? When to apply pseudo-well? What are the uncertainties in reservoir modeling?
Earth models for early exploration stages PETROLEUM ENGINEERING ÂNGELA PEREIRA Introduction Frontier basins and unexplored.
Geologic Maps Geologic Principles Original horizontality Superposition
Geologic Maps Geologic Principles Original horizontality Superposition
Structural Analysis - What is it?
Seismic Facies Analysis
Observed and predicted P wave arrivals
Geologic Maps Geologic Principles Original horizontality Superposition
Oil or Gas??? Should there be a difference in seismic response (AVO) between an oil-filled reservoir and a gas-filled reservoir? Model response with different.
of these basic elements
Outline Review causes of seismic response
Outcrop Studies (age-equivalent or analogs)
Seismic attribute applications:
Coherency Data Also known as Discontinuity or Variance
DHIs: Amplitude Anomalies
Exercise 6b: Frequency & Wavelength
Thin beds have almost no impact due to destructive interference
Chronostratigraphy Units defined based on time-equivalent stratal surfaces, natural stratigraphic subdivisions Chronozones vary in space but not time Correspond.
What Is Seismic Facies Analysis?
Seismic Interpretation
Objectives of Well-Seismic Ties
Seismic - Units 10s of Meters Thick
The Convolution Method
Stratigraphic Traps – Sub-Unconformity & Reef
Terminations: Base of a Sequence
Thud! Ring! Seismic Response What causes a seismic response?
Do Steps From Area to Volume Volume of a Cone = 1/3 Π r2 * h
How Can We Define Stratal Units?
Let’s say our trap in cross-section view looks like this….
A Predicted Porosity Map
Example: Nearshore Sands
Posting Geometric Observation
Seismic-Well Tie Flow-Chart
The STRENGTHS of Seismic Data
Reservoir Simulation FEEDBACK INPUT Geologic Model Time
A Geologic Model 1m 75 m Perm 250 mD Sand Shale 0.1 mD 50 m Slide 16
Comparison of Seismic and Well Data
Causal (real – no motion before wave arrives) Front loaded
Seismic Line Across ‘Alpha’
Well Log Correlation Well logs give us detailed information at the location of the borehole If there are several wells in an area, we can correlate stratigraphic.
Local Data - Subsurface
Shot Gather For Shot 1 Source Receivers R1 R2 R3 R4 R5 S1
Seismic Facies Mapping Exercise
Caliper Logs What Do They Measure? How Do They Work?
Modeling the seismic response:
Fault Identification: Time Slice View
Changes in Amplitude Indicate Fluid
The Ideal Seismic Response
Classes of seismic attributes?
From Raw Data to an Image
Seismic Reflections Lecture Shot Receiver Seismic Record
АВЛИГАТАЙ ТЭМЦЭХ ҮНДЭСНИЙ ХӨТӨЛБӨР /танилцуулга/
Midterm Exam Closed book, notes, computer Similar to test 1 in format:
Reshot for Development
Limited to Mapped Horizons Regular Intervals as Defined by the User
Presentation transcript:

Purposes for Well-Seismic Ties & Quality Business Stage Accuracy Required Seismic Quality Required Example Application Regional Mapping Within a few cycles Within ~½ cycle Wavelet character match Poor/fair Good Very good Mapping and tying a regional flooding surface across a basin Exploration Comparing a lead to nearby wells Exploitation Seismic attribute analysis Inversion SLIDE 4 The purpose and required accuracy of a well-seismic tie varies with the stage of our studies If we are doing regional mapping, e.g., mapping a significant erosional unconformity or a flooding surface, then our tie does not need to be very precise, within 1 or 2 seismic cycles (peaks or troughs) – and the seismic data quality does not have to be very good In the exploration stage, we would like to tie well data, e.g., the top of a stratigraphic horizon/marker within ½ a cycle This requires good seismic data quality In the exploitation stage (development & production), we need to not only know the seismic event within ½ a cycle, but the shape of the real and modeled seismic trace should be quite similar For this, we need very good seismic data quality If we obtain a good character (shape) tie between the real and synthetic traces, then: We would then be able to extract various seismic attributes (measures of the seismic wavelets) to predict rock and fluid properties We may also be able to use a process called inversion to transform the seismic data into an estimate of the rock properties in cross-section views or as a 3D volume (if we have 3D seismic data) Courtesy of ExxonMobil L 7 – Well-Seismic 1