vtem airborne em system clearly detects abra polymetallic ... et al...abra survey date 2012 1996...
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![Page 1: VTEM airborne EM system clearly detects Abra polymetallic ... et al...Abra Survey Date 2012 1996 2011 Configuration In Loop Towed Bird In Loop Frequency (Hz) 25 25 25 Terrain Clearance](https://reader036.vdocument.in/reader036/viewer/2022081411/60aeda8e71e198181c42ce8a/html5/thumbnails/1.jpg)
A Practical One-Day Workshop on Airborne Electromagnetics, November 2012
VTEM airborne EM system clearly detects
Abra polymetallic base metal deposit;
an ongoing comparison to other airborne
and ground EM systems
J. Meyers, J. Wood, D. Stannard and N. Cantwell: Resource
Potentials Pty Ltd
Keith Fisk: Geotech Airborne Pty Ltd
M. Wang and L. Hardy: Abra Mining Pty Ltd
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• Abra is a SEDEX (Sedimentary
Exhalative) deposit
• Discovered in 1981 by drilling a
blind coincident magnetic and
gravity anomaly to over 250m depth
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• Upper Stratabound zone main source of magnetic anomaly with
MAGNETITE alteration and some PYRRHOTITE, underlain by
HEMATITE alteration
• Entire mineralised zone contains some BARITE alteration, iron oxide
minerals with minor Pb and Cu sulphides which contribute to gravity
anomaly
• Deep base metal deposit still in the ground and is free of cultural
interference – Excellent geophysical testing ground
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Abra
• Lies within the
Former
Bangemall
Basin
• Now the
Edmund and
Collier Basins
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ABRA
West Creek Fm
Gap Well Fm
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REPRODUCED FROM VOGHT AND STUMPFL, 1987
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Aeromagnetics Gravity
Abra Orebody Wireframe
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AEM - VTEM Ground EM - SIROTEM
Abra Orebody Wireframe
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1
2 4 +py/gal
5 6
7
8
9
10
11
1
4
5
6
7
8
9
10
11
3
3 carbonate + gal, py
1.E-02
1.E-01
1.E+00
1.E+01
1.E+02
1.E+03
1.E+04
1.E+05
1.E+06
0.0 0.5 1.0 1.5 2.0 2.5 3.0 3.5 4.0 4.5 5.0
ro 1
kH
z (
sat)
oh
m m
apparent porosity, PA, %
Fig Rsat vs PA
NOTE THE
ANISOTROPY
max
min
Archie Equations, theoretical,
clean formations,
sat. saltywater rw = 1 ohm m
ro = F rw, F = PA-2
ILLUSTRATIVE, NOT DEFINITIVE
barite +gal +/- py
banded mtt
barite gal + qtz
jaspilites
conductive solids (sulphides, mtt)
NOTE THE LOW POROSITIES
SYSTEMS EXPLORATION (NSW) PTY LIMITED
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GEOTEM – Geoterrex / Fugro XTEM - GPX
VTEM Plus - Geotech
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System VTEM Plus Geotem Deep XTEM
Abra Survey Date 2012 1996 2011
Configuration In Loop Towed Bird In Loop
Frequency (Hz) 25 25 25
Terrain Clearance (m) 25 60 35
Tx Dipole Moment (Am2) 403506 696000 103200
Waveform Trapezoidal Half Sinusoid
Square Wave
25% Duty Cycle
Number Off Time Channels 35 16 30
Latest Channel Time
Centers (ms) 9.286 14.486 11.733
Components
Z & X
dB/dt & B Field
Z & X
dB/dt (3 comp B
Field now vailable)
Z
dB/dt
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0
200,000
400,000
600,000
800,000
0 5 10 15 20
Mo
men
t (A
m2)
Time (ms)
Airborne EM Waveforms
VTEM
GEOTEM
XTEM
0
200,000
400,000
600,000
800,000
0 5 10 15 20
Mo
men
t (A
m2)
Time (ms)
VTEM Plus
Waveform
Reciever Sampling
0
200,000
400,000
600,000
800,000
0 5 10 15 20
Mo
men
t (A
m2)
Time (ms)
GEOTEM Deep
Waveform
Reciever Sampling
0
200,000
400,000
600,000
800,000
0 5 10 15 20
Mo
men
t (A
m2)
Time (ms)
XTEM
Waveform
Reciever Sampling
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VTEM Plus
Ch 35 B Field GEOTEM Deep
Ch 15 dB/dt XTEM
Ch 20 dB/dt
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ABRA
VTEM Plus – 2012
(Geotech)
GEOTEM Deep – 1996
(Geoterrex / Fugro)
XTEM – 2011
(GPX)
S N S
N
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Early delay time
Late delay time
Dip = 90
Dip = 45
Dip = 0
B
z/
t (m
V/A
)
B
z/
t (m
V/A
)
B
z/
t (m
V/A
)
Asymmetric response
• Abra – Dipping approx 30 S o
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Z Component – B Field X Component – dB/dt S N S N
• Preliminary
data
• Good mid – late
time response
ABRA ABRA
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Z Component – dB/dt X Component – dB/dt S N S N
• Weak mid - late
time response
ABRA ABRA
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Z Component – dB/dt S N
• No detectable
response
ABRA
X
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ABRA
SmarTEM - 2006
(200m In Loop)
S N S
N
SIROTEM - 1982
(200m Coincident Loop)
FLEM - 2006
(Single Large Loop)
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S N ABRA S N ABRA S N ABRA
2006 MLEM 1982 MLEM 2006 FLEM
• Good Mid to late time EM response, but still decays away at late times
• Only moderately conductive overall
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S N ABRA
Z Component
S N ABRA S N
ABRA
X Component Y Component
• Preliminary data to date, received last night
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S N ABRA
• Preliminary results to date
• Z Component dB/dt
Conductivity Depth Image
• Good correlation to known
mineralisation
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N
• Westerly view of CDI
and known
mineralisation
• Good correlation to
depth
• VTEM likely “seeing”
the upper mineralised
zone
S
VTEM CDI
Voxel
Abra 3% Pb
grade shell
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N • NE view of DHEM and
known mineralisation
• Locally some high
conductivities
• Complex conductivity
regime
• Possibly due to
brecciated sulphide
zones, giving a poor
overall EM conductor
S
Abra 3% Pb
grade shell
Abra 3% P
grade shell
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N
Westerly view of IP Section and known mineralisation
S
Inverted IP
Chargeability
model
Abra 3% Pb
grade shell
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Scope for more AEM (VTEM) exploration in the area based on
fantastic results at Abra
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NORTH SOUTH
1000m
0m
500m
400 CHANNELS, 5m SHOTS+RECEIVERS, DEPTH MIGRATED
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• Abra is a good deep geophysical test range
-Clean and still in situ
• Clearly detected by the VTEM plus system
• Locally has high conductive zones but overall is only moderately conductive
FUTURE WORK
TEST OTHER AEM SYSTEMS:
• HeliTEM – Fugro
• SpectrEM – Anglo
• VTEMmax and VTEM 35m – Geotech Airborne
• ZTEM – Geotech Airborne
More EM – MT, AMT
3D Seismic
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A Practical One-Day Workshop on Airborne Electromagnetics, November 2012
VTEM airborne EM system clearly detects
Abra polymetallic base metal deposit;
an ongoing comparison to other airborne
and ground EM systems
J. Meyers, J. Wood, D. Stannard and N. Cantwell: Resource
Potentials Pty Ltd
Thanks to:
Keith Fisk: Geotech Airborne Pty Ltd
M. Wang and L. Hardy: Abra Mining Pty Ltd