Objectives of Well-Seismic Ties

Slides:



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

Wedge Modeling HRS-9 Hampson-Russell Software
Seismic Stratigraphy EPS 444
What is a reflector? There are many reflectors on a seismic section. Major changes in properties usually produce strong, continuous reflectors as shown.
Establishing Well to Seismic Tie
Geology 5660/6660 Applied Geophysics 24 Feb 2014 © A.R. Lowry 2014 For Wed 26 Feb: Burger (§8.4) Last Time: Industry Seismic Interpretation Well.
G P Non-Conforming Sands Type -4 Type -5 Negative 0 Positive Type -3
Investigation of Subsurface Magma Feeders Taryn Serwatowski Dr. Sven Morgan Department of Geology CMU.
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.
Advance Seismic Interpretation Project
I. Basic Techniques in Structural Geology
Single fold vs. Multi-fold CMP seismic profiling
Small scale reflection seismology
Applied Geophysics Fall 2016 Umass Lowell
Raw Seismic Data For the explosion we just considered ...
Progradational Internal Configurations
Reservoir Characterization in Leming Lake, Alberta
Porosity Logs Shale Density porosity (solid black line)
of these basic elements
Acoustic Structure of the Earth
Sonic (Velocity) Logs Sonic (DT)
A A Doesn’t Tie Shoe Lace - Comparison START Assume you travel at
 The Seismic Method .3 s .1 s .5 s 0 s .2 s .4 s .6 s .7 s .8 s 0 s
Seismic Processing Data Processing Stream Field Record (marine)
Acoustic Reflection 2 (distance) = (velocity) (time) *
Elements of 3D Seismology: Introduction to Interpretation
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
The Wave Equation Modeled
Seismic - Units 10s of Meters Thick
The Convolution Method
Purposes for Well-Seismic Ties & Quality
Summary: Lateral Resolution
Thud! Ring! Seismic Response What causes a seismic response?
From Raw Data to an Image
A Predicted Porosity Map
Example: Nearshore Sands
Seismic-Well Tie Flow-Chart
The STRENGTHS of Seismic Data
Comparison of Seismic and Well Data
Well Measurements: Wire-line Logs
Measurements In Time and In Depth
Typical Vertical Resolution
Packet #4 Definition of the Derivative
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
A Prospect A prospect is a location and depth that has been identified as a good place to drill for oil and/or gas For us to find oil or gas, certain conditions.
Shot Gather For Shot 1 Source Receivers R1 R2 R3 R4 R5 S1
Seismic Facies Mapping Exercise
Raw Data - Marine SLIDE 6 Here is a display of raw seismic data – what would be recorded for one shot/explosion (marine example) The horizontal scale is.
Petroleum System Elements
Most-Likely Scenario Present Oil & Gas Oil Gas Alpha Beta Overburden
Vertical Resolution Gamma Ray
Modeling the seismic response:
Fault Identification: Time Slice View
The Ideal Seismic Response
DHIs: Fluid Contacts Hydrocarbons are lighter than water and tend to form flat events at the gas/oil contact and the oil/water contact. Thicker Reservoir.
Good Migration Enhances Resolution
Classes of seismic attributes?
From Raw Data to an Image
Well Correlation Exercise
Seismic Reflections Lecture Shot Receiver Seismic Record
      Time for an Exercise Where would the reflection lie? 1 2 3
Limited to Mapped Horizons Regular Intervals as Defined by the User
EXPLORATION GEOPHYSICS
The nice looking seismic sections you’re used to seeing in text books are compiled from field data which is collected in the form of shot records. The.
Packing of uniform spheres
Presentation transcript:

Objectives of Well-Seismic Ties Well-seismic ties allow well data, measured in units of depth, to be compared to seismic data, measured in units of time This allows us to relate horizon tops identified in a well with specific reflections on the seismic section We use sonic and density well logs to generate a synthetic seismic trace The synthetic trace is compared to the real seismic data collected near the well location Synthetic Trace SLIDE 3 The objectives for performing a well-seismic tie are listed here Wells, of course, are registered in units of depth – feet or meters Seismic data is recorded and usually worked with a vertical scale of 2-way travel time To relate well data to seismic data, and vice versa, we have to handle this change in vertical scale units Thus: Well-seismic ties allow well data, measured in units of depth, to be compared to seismic data, measured in units of time This allows us to relate horizon tops identified in a well with specific reflections on the seismic section We use sonic and density well logs to generate a synthetic seismic trace The synthetic trace is compared to the real seismic data collected near the well location The well-seismic tie is the bridge we need to go from seismic “wiggles” to the rocks that produced the “wiggles” and our interpretation of the subsurface geology Courtesy of ExxonMobil L 7 – Well-Seismic 1