Title: Interferometric Multiple Migration of UPRC Data
1Interferometric Multiple Migration of UPRC Data
- Jianhua Yu
- University of Utah
2 ? Motivation and Objective ? Interferometric
Migration Crosscorrelogram migration
Autocorrelogram migration ? Examples
Synthetic Data UPRC data ? Summary
Outline
3 Motivation and Objective ? Interferometric
Migration Crosscorrelogram migration
Autocorrelogram migration ? Examples
Synthetic Data UPRC data ? Summary
Outline
4IVSPWD Objective
- ? Provide Look-ahead Image Below Drill Bit
- ? Reduce Uncertainty in Drilling
-
?
5Problem
? No Source Wavelet ? No Source Initiation
Time ? Not Easy to Get Pilot Signal in
Deviated Well
6Solution
Interferometric Migration
No need to know source wavelet
No need to know source location
No limits to deviated well
No need to know initial time
7 Outline . Motivation and
Objective . Interferometric Migration .
Examples . Summary
8 . Crosscorrelogram migration .
Autocorrelogram migration
Interferometric Migration
9Well
Receiver
Ghost
Direct Wave
Primary
Drill bit
Primary, Ghost and Direct Wave
10Free-surface related Ghost Travel Time
g
g
s
x
11Ghost Imaging Condition After Correlation of
Traces
Condition recording data have to be dense !!
12Crosscorrelogram Ghost Imaging Condition
13Crosscorrelogram Migration
14 . Crosscorrelogram migration .
Autocorrelogram migration
Interferometric Migration
15Free-surface related Ghost Travel time
g
g
s
x
16Autocorrelogram Ghost Imaging Condition
g
g
s
x
17Autocorrelogram Migration
18 Outline . Motivation and
Objective . Autocorrelogram Migration
Method . Examples . Summary
19Geological Model
X (m)
4
0
0
V1
V2
Depth (m)
V3
V4
V5
V6
3
20Velocity Model
X(km)
X(km)
0 4
0 4
0
0
3.5
3.5
Depth(km)
2.0
2.0
3
3
Interval Velocity
RMS Velocity
21Shot Gather and Crosscorrelogram
Traces
Traces
1 200
1 200
0
0
Time (s)
Time (s)
4
4
CSG 10 and Master trace at 80
22Shot Gather and Autocorrelogram
Traces
Traces
1 200
1 200
0
0
Time (s)
Time (s)
4
4
CSG 10
23Crosscorrelogram Migration Results
X (km)
X (km)
1.6 2.1
1.6 2.1
0
Time (s)
2.2
With primary
Without primary
24Autocorrelogram Migration Results
X (km)
X (km)
1.6 2.1
1.6 2.1
0
Time (s)
2.2
With primary
Without primary
25Acquisition Survey
East (kft)
0
4.5
0
Drill bit
North (kft)
Well Rig
3C Receivers
-5
0
Depth (kft)
10
26Main Acquisition Parameters
Drill-bit Depth 9188 ft Offset Range
1135-4740 ft Recording Length 20
s Sample Interval 2 ms Station Number
10
27Drill-bit Data of CSG 96
Trace Number
1 10
0
Time (s)
7
28Main Processing Steps
Trace editing and static shift
Frequency panel analysis and noise elimination
Amplitude balance and energy normalization
Velocity analysis
Calculating cross- and autocorrelograms,
vertical stacking
Cross- and Autocorelogram migration
29Frequency Panel Analysis
1 10
1 10
0
0
Time (s)
Time (s)
7
7
5-15 Hz
lt 5 Hz
30Frequency Panel Analysis
1 10
1 10
0
0
Time (s)
Time (s)
7
7
25-40 Hz
15-25 Hz
31Processed CSG 96 Part of CRG 6
1 10
1 13
0
0.5
Time (s)
Time (s)
7
4.5
32Crosscorrelogram of CSG 96
Trace No.
1 10
1 10
1 10
0
Time (s)
4
12 s
16 s
8 s
33Autocorrelogram of CSG 96
1 10
1 10
1 10
0
Time (s)
4
12 s
16 s
8 s
34Autocorrlogram Migration Images
Traces
Traces
1
50
1
50
0.5
Time (s)
3.2
Window 8 s
Window12 s
35Crosscorrlogram Migration Images
Traces
Traces
1
50
1
50
0.5
Time (s)
3.2
Window 8 s
Window12 s
36Acquisition Survey Map
Well Rig
0
Line AC4
North (ft)
Drill bit
3C Receivers
-5000
0
1500
3000
4500
East (ft)
37SP
1255
1215
1235
1.0
Drilling hole
Time (s)
2.0
3.0
Autocorrelation Ghost Image(Corr. Window8 s)
38SP
1255
1215
1235
1.0
Drilling hole
Time (s)
2.0
3.0
Crosscorrelation Ghost Image ( Corr. Window 12 s)
39 Outline . Objective .
Autocorrelogram Migration . Examples .
Summary
?
40SUMMARY
41SUMMARY
Difficulty of separating upgoing and downgoing
wave can cause artifacts in migration image
42Whats Next
Improve the methods efficiency for real-time
purpose
Reduced the virtual multiple and other waves
influence
Integrated migration image of both borehole data
and CDP data
43Acknowledgements
- I greatly appreciate Union Pacific Resources for
donating this data - I am grateful to the 2000 sponsors of the UTAM
consortium for financial support - I also thank all of people who give me some
suggestions and help for this work