state-of-the-art in passive seismic array methodology, and ... · why arrays? techniques...
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State-of-the-art in passive seismic array methodology,
Nick Smith PassiveX Pty. Ltd.
And useful application for mineral exploration
Overview Wavefield Why arrays? Techniques Applications
l Microtremor wavefield l Why use arrays? l Array techniques l State of the art methodology l Applications
Overview
Microtremor Wavefield
Microseism
Microtremor
Central Australia North Chile Overview Wavefield Why arrays? Techniques Applications
Surface Waves
Time
Offset
Surface waves Decay = 1/r
Body waves Decay = 1/r2
Overview Wavefield Why arrays? Techniques Applications
Surface Waves
Overview Wavefield Why arrays? Techniques Applications
Bensen et.al. (2007)
Surface Waves
Overview Wavefield Why arrays? Techniques Applications
Love Waves Rayleigh Waves
Depth
Sensitivity
10 Hz
5 Hz
1 Hz
Surface Waves
Overview Wavefield Why arrays? Techniques Applications
Surface wave phase velocity sensitive to seismic
velocity structure (Vp, Vs and Density) l Most sensitive to Vs l Vs insensitive to fluids (e.g. groundwater)
Why Use Arrays?
Overview Wavefield Why arrays? Techniques Applications
l Fundamental information on cover! − Cover +/- bedrock velocity structure − Stratigraphic variability
Techniques
Overview Wavefield Why arrays? Techniques Applications
Array concepts: l Seismic interferometry
— Retrieve coherent wavefield propagating between
two sensors — Greens function
l Array beamforming — Delay and sum, power distribution
— Wavefield composition, directionality and velocity
Array Techniques
Overview Wavefield Why arrays? Techniques Applications
SPAC l Circular array, 4+ sensors l Ave. coherency for sensor pairs l Independent of wavefield directionality l Surface wave dispersion
l Shear-wave velocity vs depth.
Array Techniques
Overview Wavefield Why arrays? Techniques Applications
SPAC l Cross correlation / coherency
l Isotropic wavefield OR azimuthal average
Azim. Ave. coherency
Coh
eren
cy
Frequency
Coherency
Array Techniques
Overview Wavefield Why arrays? Techniques Applications
SPAC
l Sensor separation → wavelength sensitivity
r1 r2
r3 r4
Array Techniques
Overview Wavefield Why arrays? Techniques Applications
FK
l Complex array design, 10+ sensors
l Array beamforming
l Wavefield characterisation
l Velocity vs depth
Array Techniques
Overview Wavefield Why arrays? Techniques Applications
FK
l Array design and array response
Kennett, et.al. (2015)
Array Techniques
Overview Wavefield Why arrays? Techniques Applications
FK
l Array response steering by coherent signal
— Basic concept: delay and sum of signals
— In practise: calculate power for different
combinations of back azimuth and slowness
Array Techniques
Overview Wavefield Why arrays? Techniques Applications
PSAR SQspa
Kennett, et.al. (2015) FK
Array Techniques
Overview Wavefield Why arrays? Techniques Applications
Gal, et.al. (2014)
FK
Array Techniques
Overview Wavefield Why arrays? Techniques Applications
State of the art methodology
l Three component constraints
Love Waves Rayleigh Waves
Depth
Sensitivity
Array Techniques
Overview Wavefield Why arrays? Techniques Applications
State of the art methodology
l Inversion techniques
— e.g. Neighbourhood Algorithm
— e.g. Markov Chain Monte Carlo NA Velocity versus Depth
Array Techniques
Overview Wavefield Why arrays? Techniques Applications
State of the art methodology
l Markov Chain Monte Carlo
— Bayesian inference
— Correct propagation of uncertainty into modelling
result
— Does not require explicit regularisation or
parameterisation
— Trans-dimensional
Array Techniques
Overview Wavefield Why arrays? Techniques Applications
State of the art methodology
l Markov Chain Monte Carlo
Bodin, et.al. (2012)
Applications
Overview Wavefield Why arrays? Techniques Applications
Turning noise into signal is really interesting
BUT….. Why is this important for mineral exploration?
Applications
Overview Wavefield Why arrays? Techniques Applications
1. Shear wave velocity vs depth profiles for
greenfields passive seismic work
2. Assessment of the changeability of “1)” throughout the project area
3. Assessment of complex geology
4. Assessment of complex wave propagation phenomena for best modelling results
Applications
Overview Wavefield Why arrays? Techniques Applications
1) and 2): Average Vs variation
- H/V resonance frequency depth conversion
- Geological structure
Applications
Overview Wavefield Why arrays? Techniques Applications
3) Complex geology
- Multiple large impedance contrasts
- Velocity inversion El
liptic
ity
Azi
. Ave
. Coh
Depth (m
)
50
150
Stra
tigra
phy
500 1500
SPAC SPAC + H/V
Vs (m/s) Frequency (Hz)
Applications
Overview Wavefield Why arrays? Techniques Applications
4) Complex wavefield - Higher modes - Sites with large Vs contrasts, or velocity reversals - Source characteristics
n = 1 n = 2 n = 4
niV < ni+1
V < ni+2V...
Applications
Overview Wavefield Why arrays? Techniques Applications
Higher modes SPAC using model based “effective mode” and amplitude response for assumed harmonic vertical point sources
Ikeda, et.al. (2012)
Summary
Overview Wavefield Why arrays? Techniques Applications
Passive seismic arrays are not just interesting... They are also useful for: l Characterising the wavefield l Characterising the geology l Validating assumptions And are critical for l Accurate and adaptive large scale passive seismic
surveying