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.

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.
Dolch Words.
5 Why’s Overview.
H.S. Physical Science Chapters 1 and 2
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.

Seismic noise is omnipresent The next slide goes back to earlier work where the shear problem became apparent. It curls around our reflection events, Enhancing.
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
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.
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.
Click here to enter. Click a menu option to view more details Starters Main Courses Desserts Click on the coffee cup to return when Navigating For Vocabulary.
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.
1 Aggregate Supply The AS is the part of our national economy model where the production side is studied.
? 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.
GG450 April 22, 2008 Seismic Processing.
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,
GG 450 April 30, 2008 Seismic Reflection Interpretation.
Reflection Field Methods
Production In this section we want to explore ideas about production of output from using inputs. We will do so in both a short run context and in a long.
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.
What to do when you are done. PRINTING WITH PHOTOSHOP.
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.
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.
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.
1 What NOT to do I get sooooo Frustrated! Marking the SAME wrong answer hundreds of times! I will give a list of mistakes which I particularly hate marking.
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.
40 Multiple Choice Items TIMED! 35 Minutes Data Representation (38%) Research Summaries (45%) Conflicting Viewpoints (17%) Content Includes: Biology,
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.
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.
Photography has played a significant role in our society and continues to, especially today. If you stop to think about it, photography has perhaps even.
CMPF144 FUNDAMENTALS OF COMPUTING THEORY Module 10: Applied Mathematical - Logical Knowledge Riddle/Puzzle.
WHY DO WE LOOK FOR FAULTS?? Geologists of the end of the 19th century (at that time geologists were more like adventurers rather than scientists!) realized.
Grade Book Database Presentation Jeanne Winstead CINS 137.
Tom Wilson, Department of Geology and Geography Environmental and Exploration Geophysics II tom.h.wilson Department of Geology.
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.
Sight Words.
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.
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.
Data QC and filtering Bryce HutchinsonSumit Verma Objective: Consider the frequency range of different seismic features Look for low frequency and high.
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.
1 Geophysical Methods Data Acquisition, Analysis, Processing, Modelling, Interpretation.
A history of misguided pre-stack processing.
Applied Geophysics Fall 2016 Umass Lowell
PowerPoint Xpress Start
Modeling of free-surface multiples - 2
From Raw Data to an Image
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.
5 Why’s Overview.
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.
—Based on 2018 Field School Seismic Data
From shale play To Gulf coast prospects
Presentation transcript:

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 screen, each gather trace had to be shifted by the amount computed from the linear refraction slope illustrated on the previous slide. These slopes are very extreme (ranging upwards to a couple thousand samples per spread). As I said, without correction you wouldn’t see the events at all, yet here they show their intractable truth. I am sure this explains why nobody has done this type of removal before. In any case I cut them out to save space. I just chose these few (out of the hundreds the system lifted off) to make the following crucial points: 1. No shaping after the fact was used, so, as I say above, the mere presence of these obvious events, way into the spread, is firm logical proof that they are coherent noise and that they will affect the stack. The fact that my logic does not see them on it’s next iteration is internal verification that they have all been effectively removed. This passes the programmer honesty test. 2.The last 5 start from within the band of noise the industry commonly attributes to ground roll. As the system removes event after event, this strong inside band gets eventually (almost) eliminated. Again this proves this overpowering energy is traveling vertically through the section (shear wave) rather than along the surface (ground roll). So this is what my logic removes from the gathers. I mentioned the nature of the task was such that all the shot points affecting a gather had to be treated before final answers could be prepared (and that is a bunch). Watching the system removing tons of energy from the data made me wonder if anything would be left. To find out we now jump into those final results and see the answer is a strong yes! Just keep in mind that the detected noise was generally a lot stronger than the signal, even way into the spread.

A deep well to the south of this Louisiana salt dome project project indicates that the prolific shale play strata I show below extends into this area. The well log match comparison comes from work I did up North. The deep stratigraphic pinch-out we see on my noise removal results (to the right) does not even appear on the unresolved input. There’s no way my system could have invented that. No one thought to tell my system this was a salt dome project. It took it upon itself to delineate the outlines of the dome. The green delimiter is mine, of course. In the main results report you will see many examples where noise loops over this boundary. I have included one on the final slide here. At interpretation time what the system takes out is often as important as what it uncovers. The next slide continues this thought. Honest continuity is another form of proof. While migration mixes heavily, every trace here is completely independent, They all go through the same manipulations, but never are aware what is going on next door. So when you see strong events that did not even show up before, and when these events make great geologic sense there evolves a truth that defies words. What is even more crucial is the knowledge of how much energy was lifted off before these reflections became visible.

Closing out the double intro – To begin, the green delineation line is in the same place on both. I just cut off the rest of the salt to save space. So let me just cover several points of interest. 1. Unfortunately the strong apparent dips at the edge of the dome were the geologists target. The system threw them out to his intense displeasure. 2. Careful study shows the dips and the events are not the same. This introduces the problem of close overlap of noise and signal, probably the primary challenge to the logic. 3. Point 2 applies here in spades (meaning extremely). Here we see the noise continuing into no-mans land. 4. Both points strongly apply here.To the left of the demarcation, where there is virtually nothing showing on the input, our results are strong. To the right we see nothing, meaning the input was pure noise. Now, reasonable people should see we are dealing with a major discovery here – one that opens new exploration possibilities. (at least that is how it seems to me.)

Allow them time to load! A PowerPoint compendium of seismic topics Basic reflection theory the experts seemed to have missed. Inversion and integration – the all important sonic log simulation. Coherent noise background – an explanation of types. Removal of coherent noise on Gulf Coast – a breakthrough. Vibroseis de-noising – another (but similar) breakthrough. Strike slip faulting – salt dome association – new thinking. North Sea strike slip interpretation – the importance of resolution. About Paige - MS in geology,spent 7 years in Venezuela for Mobil,& then Phillips Maracaibo interpretation found Phillips’ major field there. Back to states, joined Phillips computing, became project manager for exploration. Hired by Western Geo. To start digital operations in Shreveport. Wrote first predictive deconvolution program that put Western on the map in digital processing (and formed the non-linear basis for later ADAPS software), After brief sojourn in commercial processing (where he wrote a table driven programming system), joined Dresser Olympic as both manager of processing and of research. Went on his own to start non=linear development. Consulting package consists of Paige’s personal time, his open-ended software and use of his processing hardware. Unless full segy detail is requested (segy output), the product is a series of PowerPoint studies. He can be reached at