Going for the RED is an approach used by older interpreters. But for red to indicate hydrocarbons (like this example), lots of things have to be true that.

Slides:



Advertisements
Similar presentations
Proving ADAPS via honest results. No well data is input
Advertisements

North Sea faulting How the ADAPS inversion / integration clarifies the strike-slip structure – by David Paige This study was originally proposed September,
Introducing the piggy back noise problem. This is what we saw visually on the 3D gather data. Strong and persistent cps waves riding on very low.
From shale play To Gulf coast prospects There are timed topics on many slides. An “end” message will inform you when the slide is done. The show discusses:
1.The seismic energy continuum consists of thousands of independent primary reflections, each coming from a single reflecting interface. 2. There is no.
? Mapping of gulf coast strike slip faults To the left is a set of associated strike slip and adjustment faults on the Lousiana coast. The section itself.
In the next series I present this set of cutouts and try to explain that each shows a refraction event that was lifted off. To see the events on the full.

From shale play To Gulf coast prospects There are timed topics on many slides. An “end” message will inform you when the slide is done. The show discusses:
Seismic Stratigraphy EPS 444
I was there when it all happened, a long time ago. Of course I was on the opposite side commercially. Time series limitations - Frequency domain methods.
Going for the RED is an approach used by But for Red to indicate hydrocarbons (like this example) lots of things have to be true. The project I use for.
Copyright © 2010, 2007, 2004 Pearson Education, Inc. Chapter 21 More About Tests and Intervals.
Near traces or Middle traces or Far traces The A mplitude V ersus O ffset mythology. If ever a single picture could prove a negative, this one might be.
A North Sea processing & Interpretation story. The same well image was shown on both the before and after sections above. As you may have noted, it is.
North Sea Strike Slip Fault Study – The ultimate before and after. To the left you see the best the client could do on a “well-cutting” cross line. To.
The ADAPS visual approach to interpretation When Dr. Robin Westerman talked Nexen into trying ADAPS I was presented with the display of the problem shown.
? Mapping of gulf coast strike slip faults To the left is a set of associated strike slip and adjustment faults on the Lousiana coast. The section itself.
The evolution of the down wave. We hit the earth with some sort of an impact which results in a movement. Since the earth is elastic, it rebounds past.
A North Sea processing & Interpretation story. The same well image was shown on both the before and after sections above. As you may have noted, it is.
De-noising Vibroseis The contention is that the correlated Vibroseis field record (to the far left) is a mess of overlapping coherent noise and signal,
Examining your research question Each slide in this presentation plays automatically, but you will need to click the blue arrow at the bottom of the screen.
GG 450 April 30, 2008 Seismic Reflection Interpretation.
The danger is that you’ll never believe your old interpretations after viewing this show. In my main show I compare 32 in-lines before and after noise.
Toggle guide Before A tutorial on the effect of seismic noise. (Requires lots of toggling to really see how noise interacts with signal). I start with.
Another example of critical angle refraction noise.
Exercise set 3: Basic cross sections
There is a time for ultra seismic accuracy but that comes after we have located something exciting enough to look at. Since migration before stack almost.
Shale Lime Sand The argument for non-linear methods. 1 The geology 2. The reflection coefficients (spikes in non-linear lingo). 3. The down wave 4. Its.
So where does the ADAPS optimization method fit into this framework? The seismic trace equation does not fit the linear definition, since the values on.
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.
Why determining an exact waveform is next to impossible. We start at the recording point with these facts – 1. The seismic continuum consists of overlapping.
SOURCE 2006 Presentation by Luke Arntson Game Programming Optimization.
Creative Commons Attribution 3.0 creativecommons.org/licenses/by/3.0 Key Abstractions in Game Maker Foundations of Interactive Game Design Prof. Jim Whitehead.
Some background and a few basics - How my inversion works – and why it is better - How added resolution makes parallel fault picking a possibility – The.
Looping forever Reading/observing sensors (inputs) Reacting to sensors Obstacle sensors.
Excel By: Brandon Honza. Step 1 Take the CD on the table and put it into your computer. Open the Disc. Then click and drag the entire Excel folder to.
Welcome to a before and after coherent noise removal series. There is a lot to explain about what is going on here, so I am using this otherwise wasted.
A list of inversion error causes that all attribute junkies should really understand: 1.Definition of inversion – A seismic trace is the product of the.
Depth point 1 A study of the effects of early critical angle crossings. From data I (Paige) had previously processed to check out my sonic log synthesis.
Art 315 Lecture 5 Dr. J. Parker AB 606. Last time … We wrote our first program. We used a tool called GameMaker. The program we wrote causes a ball to.
Petrel Workflow Tools 5 Day Introduction Course
ADAPS optimized stack of line 401 (no inversion or integration). Please toggle with conditioned version I start with the Paige optimized stack v.s. the.
Session 4: PREPARE FOR TESTS Year 7 Life Skills Student Wall Planner and Study Guide.
Design Principles… Alignment. The Principle of Alignment states, "Nothing should be placed on the page arbitrarily. Every item should have a visual connection.
Refraction Statics Bryce Hutchinson Sumit Verma. 3D Statics display 1. Click this button on the right side of the statics window to open a 3D statics.
Solution of. Linear Differential Equations The first special case of first order differential equations that we will look is the linear first order differential.
Because noise removal is central to my later work, I start with a discussion on how intertwined coherent noise creates a random effect that confuses all.
ADAPS multiple removal demo. The upper halves of the slides in this series show the input gathers.The bottoms show the same data with multiples removed.
 In this packet we will look at:  The meaning of acceleration  How acceleration is related to velocity and time  2 distinct types acceleration  A.
Visual interpretation is still the best. You can see reservoir possibilities that have been missed, and do it at a fraction of the normal cost. The tougher.
Multiplication of Common Fractions © Math As A Second Language All Rights Reserved next #6 Taking the Fear out of Math 1 3 ×1 3 Applying.
Welcome to a wild ride through ideas. In this show I am suggesting that the multiple fractures associated with strike slip faulting can accomplish the.
How the Saudi / shale oil battle should make us stop & think. (and I don’t mean about geo-politics). The shale production reality reminds us the Saudi.
Why inversion & integration is needed to see stratigraphy.
Can we see shale fractures? Some claim to already doing it but I have my doubts. I believe I’m close, but not there yet. I’d like opinions. The section.
Probing the question of “how good can seismic get? I ask you to spend a good amount of time just looking at the amazing detail this section shows. When.
AVCE ICT – Unit 7 - Programming Session 12 - Debugging.
Info Read SEGY Wavelet estimation New Project Correlate near offset far offset Display Well Tie Elog Strata Geoview Hampson-Russell References Create New.
Copyright © 2010, 2007, 2004 Pearson Education, Inc. Chapter 21 More About Tests and Intervals.
A history of misguided pre-stack processing.
How to Start This PowerPoint® Tutorial
HERE IS AN EXAMPLE OF ONE-DIMENSIONAL MOTION YOU’VE SEEN BEFORE
How to Start This PowerPoint® Tutorial
Dynamic Programming.
Introduction to TouchDevelop
YOUR APP NAME MY APP IS GR8 MORE TEXT FEATURE 1 FEATURE 2 FEATURE 3
BEFORE AFTER Let’s start by examining this particular sonic log match. We have super-imposed it both on the input (before) and on the output (after). Some.
Think stratigraphy, This picture, all by itself, not only proves strike slip theory, but also verifies the logic used to bring out the fault detail. This.
From shale play To Gulf coast prospects
Presentation transcript:

Going for the RED is an approach used by older interpreters. But for red to indicate hydrocarbons (like this example), lots of things have to be true that were not considered a few years ago. The project used here lies off south Louisiana. It contains several “emergence / subsidence” cycles, with obvious angular disconformities. Current automatic mapping logic can’t begin to handle such complexity, and it is obvious that visual interpretation is sorely needed, especially if we have any hope of tracking the strike slip faults that probably provide much of the trapping. If this were a section of sonic well logs, we’d feel fairly safe in picking this strong event as a probable reservoir. We cannot say that about a normal section, for a host of reasons. Actually what we are looking at is a sonic log simulation from seismic data. For now I ask you to treat it as solid, since the initial point of this presentation is to illustrate how important visual interpretation is in a preliminary selection of areas of interest. Inside, I present “before and after” pairs that are set up for “toggling”. If you have never used this tool, it is worth a visit here all on its own. Toggling helps one visualize why integration flips the polarities to achieve a simulation of lithology. Multiple well log matches prove it is doing the right thing. The reasons for including these comparisons are first that they really please me, and second because it is important for you to look at the stratigraphy with some confidence that you are really seeing true lithology. Strike slip faults are caused by stretching of shallower beds reacting to deep plate movement (continental drift). They are a fact of life that is hard to deny. Because the movement is horizontal, there may be no vertical throw to facilitate picking. This means we need every ounce of resolution improvement we can get.

Sonic log from an early shale play, imposed on an ADAPS non-linear inversion (left) and on the integrated final result (right). On the log, low velocities peak to the left (red on the the display). Bed thickness is crucial to stratigraphic correlation, and correlation is the exploration geologist’s most essential tool. In reservoir work, tracking thickness is all-important. Matching sonic logs must be the ultimate goal. All inversions contain “spike guesses” from all interfaces. Unless one is able to resolve this mess in one’s mind, any inversion by itself does not provide attributes that are trustworthy. Any single interface value is dependent on both of the bounding bed velocities. In addition, a “red” from the top interface means one thing while one from the bottom means the opposite. Thus the need for integration. Of course I don’t think others can match the ADAPS non- linear inversion, but that is something else. Examination will show there is little “polarity” correlation between inversions (even mine) and the well log. One must be careful with polarities. Many observers just line up events without regard to color. Note point A where polarities are opposed (some would think this a match). While the integrated match is not perfect, it’s pretty good. Note how well the thickness agrees. As we continue with the older part of the show, be prepared to toggle. All versions of the same original data have been carefully aligned, so two fingers on two arrows is all you need to make an intelligent comparison. Spend some time on this learning experience. A

1 Direct reservoir detection - Where words fail, the well match here says it all. It proves we could have predicted the presence of this particular reservoir before the act of drilling. The project has several wells, and the matches are all quite good. No well data was used as input to our processes, but it is nice for it to illustrate my points. The stars identify what I consider a basal sand, sitting on one of several unconformities (angular disconformities that is). The ability of the system to simulate lithology was crucial in my own interpretation.

Here is well #3. It appears to be tapping below our basal sand (again identified by stars). It is interesting to note that it (the basal sand) has petered out here. This is a problem we should expect in “on-lapping” deposition. Again this is a good match, but not perfect.

A Unadulterated stack This is the raw stack on comparison #1. Please toggle with my optimized stack. Toggling hint – place one finger on the left arrow, and one on the right arrow and start playing,

A Optimized stack input Toggle back w raw Or with the final. Going back and forth here is where the time should be spent, as the integration logic rearranges computed interfaces to simulate lithology. Lobes will disappear as they get combined with their mates.

Back to input (the optimized stack) A Final result Final ADAPS result If this is your first time into the concept, your reaction might be one of disbelief when you see the shifting lobes. All I need to say here is that the well matches are not lying, and there is no way I could make them up. The fact that normal seismic sections don’t represent lithology is worth knowing.

YYYY straight stack Toggle with the optimized stack. But first notice where the arrow is pointing. Straight stack

The optimized stack You should notice glimpses of the basal sand to the right of the arrow. Of course this becomes the input to the inversion/integration logic. Toggle back to the simple. Or toggle with the final Optimized stack

Amazing if true – (and we sure think it is). What we see repeated in this toggle trio is a serious case of tuning and subsequent de- tuning. The basal sand we see here (which checks out on other lines) hardly shows up before NLI. Final inverted and integrated

toggle with the optimized stack. Straight stack Another example.

The optimized stack Again notice that the basal sand is visible now, before inversion. In particular, really look at the right-hand arrow. Toggle back to the simple. Or with the answer Optimized stack

Final inverted and integrated Toggle with the optimized stack.

In-line XX6 and cross-line 2900 I close the toggling session with a right angle intersect to show the merit of visualizing complex results. These were two completely separate runs, using the same parameters Of note here is the “bright spot” verification we get when the hydrocarbon indication fades down dip.. the fact that these two runs tie beautifully builds confidence in the total system. Click to start over and really toggle this time. Or here to repeat the last series. Or here to return to base. Or here to start strike slip discussion.