geo 395 - module 12 Flashcards

1
Q

true stratigraphic nature of seismic reflections

A
  • acoustic impedance changes are assumed to be parallel to bedding
  • no consideration to amplitude and waveshape variations
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2
Q

origins of petroleum reservoirs and traps

A
  • structural traps (fold - syncline, anticline) and unconformities
  • stratigraphic traps (reefs and sand bodies)
  • combination traps (salt domes!)
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3
Q

Convolution model of seismic trace using zero phase band-pass wavelet

A

KNOW THE DIAGRAM

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4
Q

Summary - How to – reflection identification

A

pick a survey by tying strong reflections on lines through wells in VSPs, synthetic seismograms or sonic logs. From velocity and density log convolved with source wavelet.

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5
Q

Mis-ties and causes (in acquisition)

A
  • seismic source type
  • field filter
  • sample rate
  • field polarity
  • vintge
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6
Q

Mis-ties and causes (in processing)

A
  • deconvolution
  • statics (refraction and residual statics)
  • velocities
  • 2D
  • vintage
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7
Q

workstation interpretation - recipe

A
  • collect data
  • scan for QC, polarity, data structure and stratigraphy)
  • tie well data
  • pick horizons and faults, loops
  • review start
  • review struct
  • map
  • ID attributes (azimuth, dip, a
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8
Q

3D seismic volume

A
IL, XL, X, Y, Z, time or depth
XY grid - bin size
Z increment (sample rate)
amplitude range
8 bit   -127  + 128   workstation
16 bit
32 bit
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9
Q

plus and minus zero-crossings

A

Make a dot at the peaks.
left side is -ve and right side is +ve
if it looks like an S then going from -ve to +ve
If it looks like inverted S the going from +ve to -ve

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10
Q

flattening - DEFINITION

A

application of a time correction to each CDP trace of a horizon such that the horizon is at a constant time

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11
Q

stratigraphic interpretation

A

horizon vsp vs. synthetic

auto picking algorithm - cross correlation algorithms. compare model trace to each individual trace being tracked.

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12
Q

structural interpretation

A

struct and strat interpretation needs to be done simultaneously
heave - horizontal displacement
throw - vertical displacement of 2 fault blocks

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13
Q

coherency

A

generated based on similarity of adjacent traces.
high coherency if v similar
low coherence if dissimilar

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14
Q

coherency coefficient

A

higher number = higher similarity

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