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Progress of the Atlantis 4C Node Project

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Analyze the P-SV converted waves in multicomponent data. Determine velocities for Vp and Vs. Observe ... QC polarity of 3C and hydrophone at the direct arrival ... – PowerPoint PPT presentation

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Title: Progress of the Atlantis 4C Node Project


1
Progress of the Atlantis 4C Node Project
  • Presented by Jeff Kao
  • M.S. Geophysics
  • Advisor Dr. Robert Tatham

2
Outline
  • Objective of research
  • Introduction to project
  • Methodology
  • Overview of research and preliminary progress
  • Summary
  • Future Work

3
Objective
  • Analyze the P-SV converted waves in
    multicomponent data
  • Determine velocities for Vp and Vs
  • Observe the occurrences of the converted waves
  • Use seismically estimated Vp and Vs to describe
    shallow pore-pressure variations

4
Introduction
  • Atlantis Field was discovered in 1998 by BP
  • Located 300km south of New Orleans in the GOM
  • Water depths range between 1300m to 2200m
  • Survey deployed 902 OBS 4C nodes

5
Survey Geometry
  • Node spacing of 426m
  • Shot spacing of 53.7m
  • Nodes arranged in a hexagonal sampling technique
  • Density of nodes is 6.36 nodes/km2

6
Atlantis Field
Beaudoin et al.
7
Shot and Node Grid Geometry
Beaudoin et al.
8
Methodology
  • Begin analysis with one node
  • Extract shots along strike of the regional
    geology extending W to E
  • Take one shot line near node extending NW to SE
  • Analyzing horizontal components
  • Observing approx. first 3 seconds of data

9
Methodology
  • Extract shots contributing to 1 node to obtain a
    2D swath
  • QC polarity of 3C and hydrophone at the direct
    arrival
  • Rotate horizontal components to radial and
    transverse
  • Velocity analysis to attain Vp and Vs values

10
Map of Nodes
N
11
Line Extending East West
12
X Raw
E
W
13
Y Raw
W
E
14
Z Raw
W
E
15
Shot Line Trending NW to SE
16
Line 21289 X Raw
SE
NW
17
Line 21289 Y Raw
SE
NW
18
Line 21289 Z Raw
SE
NW
19
Preliminary Velocity Analysis
20
X RAW
1352 1514
1904 1326
21
Y RAW
1366 1507
1880 1316
22
Z RAW
1376 1510
1864 1351
23
Summary
  • Dealing with water depth of 2050 m
  • Direct arrival at normal incidence is 1.3
    seconds
  • Observing shallow reflections
  • Asymmetric travel time

24
Future Work
  • Estimate pore pressure in the deep water
    sediments
  • Many opportunities for future students with this
    BP data set
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