geo 395 - module 12 Flashcards
true stratigraphic nature of seismic reflections
- acoustic impedance changes are assumed to be parallel to bedding
- no consideration to amplitude and waveshape variations
origins of petroleum reservoirs and traps
- structural traps (fold - syncline, anticline) and unconformities
- stratigraphic traps (reefs and sand bodies)
- combination traps (salt domes!)
Convolution model of seismic trace using zero phase band-pass wavelet
KNOW THE DIAGRAM
Summary - How to – reflection identification
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.
Mis-ties and causes (in acquisition)
- seismic source type
- field filter
- sample rate
- field polarity
- vintge
Mis-ties and causes (in processing)
- deconvolution
- statics (refraction and residual statics)
- velocities
- 2D
- vintage
workstation interpretation - recipe
- 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
3D seismic volume
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
plus and minus zero-crossings
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
flattening - DEFINITION
application of a time correction to each CDP trace of a horizon such that the horizon is at a constant time
stratigraphic interpretation
horizon vsp vs. synthetic
auto picking algorithm - cross correlation algorithms. compare model trace to each individual trace being tracked.
structural interpretation
struct and strat interpretation needs to be done simultaneously
heave - horizontal displacement
throw - vertical displacement of 2 fault blocks
coherency
generated based on similarity of adjacent traces.
high coherency if v similar
low coherence if dissimilar
coherency coefficient
higher number = higher similarity