Geological interpretations from the Paterson AEM survey Geological interpretations from the Paterson AEM survey Ian C. Roach With contributions from: A.J. Whitaker, M.T. Costelloe & N.C. Williams Onshore Energy and Minerals Division, Geoscience Australia GPO Box 378, Canberra ACT 2601
37
Embed
Geological interpretations from the Paterson AEM …Geological interpretations from the Paterson AEM survey Geological interpretations from the Paterson AEM survey Ian C. Roach With
This document is posted to help you gain knowledge. Please leave a comment to let me know what you think about it! Share it to your friends and learn new things together.
Transcript
Geological interpretations from the Paterson AEM survey
Geological interpretations from the Paterson AEM survey
Ian C. Roach
With contributions from:A.J. Whitaker, M.T. Costelloe & N.C. Williams
Onshore Energy and Minerals Division, Geoscience AustraliaGPO Box 378, Canberra ACT 2601
Geological interpretations from the Paterson AEM survey
Interpreting AEMInterpreting AEMrequires morerequires moresophisticated knowledgesophisticated knowledgeof surface and nearof surface and near--surface geology like this surface geology like this new Permiannew Permian--MesozoicMesozoicsolid geology mapsolid geology map
Geological interpretations from the Paterson AEM survey0 10050 Kilometers
Interpreting AEMInterpreting AEMrequires morerequires moresophisticated knowledgesophisticated knowledgeof surface and nearof surface and near--surface geology like this surface geology like this new indurated regolith new indurated regolith mapmap
Geological interpretations from the Paterson AEM survey
!(
!(
!(!(NIFTY
TELFER
KINTYRE
WOODIE WOODIE
Ternary RadiometricsRed: K
Green: Th
Blue: U
0 10050 Kilometers
Ternary radiometrics tells Ternary radiometrics tells us about what occurs at us about what occurs at the surface, and the surface, and serfuaceserfuaceprocess, but what lies process, but what lies underneath?underneath?
Geological interpretations from the Paterson AEM survey
Gravity can be used to Gravity can be used to interpret large scale interpret large scale density contrasts that density contrasts that may be related to different may be related to different rock typesrock types
Geological interpretations from the Paterson AEM survey
Aeromagnetics can tell us Aeromagnetics can tell us the depth to magnetic the depth to magnetic basement and give us basement and give us another view of subanother view of sub--surface rock typessurface rock types
Geological interpretations from the Paterson AEM survey
!(
!(
!(!(NIFTY
TELFER
KINTYRE
WOODIE WOODIE
0 10050 Kilometers
How do weHow do wevalidate this?validate this?
AEM can tell us about the AEM can tell us about the lateral continuation of lateral continuation of surface and subsurface and sub--surface surface materials and can be materials and can be interpreted for geology. interpreted for geology. How do we validate this?How do we validate this?
Geological interpretations from the Paterson AEM survey
Geological validation
• Drill holes: a publicly-available drill hole compilation (Roach, 2009);
• Solid geology: a compilation by Czarnota et al.(2009);
• Surface geology: the 1:1 000 000 scale Surface Geology of Western Australia (Stewart, 2008);
• 1:250 000 and 1:100 000 geological maps;• Magnetics: GA Magnetic Map of Australia;• Gravity: GA Gravity map of Australia; • Radiometrics: GA Radiometric Map of Australia
(Minty et al., 2009);• Conductivity logs
All GA data are available onAll GA data are available on--line at: line at: www.ga.gov.auwww.ga.gov.au/minerals/minerals
Geological interpretations from the Paterson AEM survey
• 4,300+ logged drill holes.
• Released as GA Record and database Roach (2009).
DrillingDrilling
Geological interpretations from the Paterson AEM survey
Drill holes vs AEM conductivity sections
5 km
300300
200200
100100
0 m ASL0 m ASL
--100100
--200200
Geological interpretations from the Paterson AEM survey
GA LEI section geological interpretation
• Line 30820, ca. 8 km north of Nifty Cu mine.
• Interpretation after Bagas (2002), Lamil 1:100,000 geology sheet.
W E
Geological interpretations from the Paterson AEM survey
Large-scale geological interpretations
• Interpretations mostly from gridded data:– GA LEI Depth Slices:
• Created by draping gridded inversion conductivity values over an elevation model;
• Represent a conductivity ‘skin’ at a certain depth from topographic surface.
– GA LEI Elevation Slices:• Removes terrain;• Represent a conductivity ‘level’ from datum.
• Grids have data under the DOI removed.
Geological interpretations from the Paterson AEM survey
• Only drawn in areas where Permian and younger fill is conductive.
• Able to visualise large palaeotopographicfeatures and some unconformities.
Geological interpretations from the Paterson AEM survey
Depth slices show Depth slices show subsurface conductivity subsurface conductivity features, Can these be features, Can these be used to map conductivity used to map conductivity surfaces?surfaces?GA LEI Depth slices
Geological interpretations from the Paterson AEM survey
!(
!(
!(!(NIFTY
TELFER
KINTYRE
WOODIE WOODIE
0 10050 Kilometers
!(
!(
!(!(NIFTY
TELFER
KINTYRE
WOODIE WOODIE
Conductivity formlinesm ASL
-100
0
20
40
60
80
100
120
140
160
180
200
220
240
250
260
280
300
310
320
340
360
380
400
0 10050 Kilometers
!(
!(
!(!(NIFTY
TELFER
KINTYRE
WOODIE WOODIE
0 10050 Kilometers
!(
!(
!(!(NIFTY
TELFER
KINTYRE
WOODIE WOODIE
0 10050 Kilometers
Depth slice Depth slice information are used information are used here to develop a here to develop a model of the model of the PalaeozoicPalaeozoic--Proterozoic Proterozoic unconformity surface unconformity surface in the Paterson regionin the Paterson region
Geological interpretations from the Paterson AEM survey
!(
!(
!(!(NIFTY
TELFER
KINTYRE
WOODIE WOODIE
0 10050 Kilometers
The PalaeozoicThe Palaeozoic--Proterozoic unconformity Proterozoic unconformity surface, shown here, is surface, shown here, is the prethe pre--Permian Permian palaeotopographypalaeotopography
Geological interpretations from the Paterson AEM survey
Geological interpretations from the Paterson AEM survey
!(
!(
!(!(WW
WW
WW
U
W
W
UU
Mn
FeFe
MnMn
MnMn
Fe
Fe
MnAu
Mn
Fe Fe
MnMn
MnMnFe
Fe
MnMn
MnMnMnMnMnMn
Fe
Fe
Au
FeFe
FeFe
Mn
MnMn
MnMn
MnMn
Mn
MnMn
Au
Cu
MnMn
Au
Mn
Li
AuAu
Mn
Mn
Mn
CuAuAuAu
AuAu
Au
AuAu
AuAu Pb
Au
HM
Cu
Ag
Au
Au
MnMn
MnCu
AuAuAu
Fe FeFe
FeFeFe
FeFe
Au
Fe
AuAuAuAu
Au
Au
Au
FlFlAu
Au
Au
AuAu
Au AuAu
Au
AuAu
AuAu
Au
Zn
CuCu
Au
Au
Au
Au
Au
Cu
Pb
Cu
Au
CuMn
CuMnCu
Mn
Cu
CuCu
Au
Cu
MnMnMn
MnMn
Mn
Cu
Cu
CuMn
Mn
Mn
MnMn Mn
CuAuAu
Au
Au
MnMnMn
Mn
AuMnMn
AuAuAu
Au
Cu
MnAu
Au
Au
AuAu
CuCu
AuAuAu
CuCuZn
Ni
Zn
CuCu
Mn
Mn
Mn
Mn
MnMn
MnAu AuAu
Cu
Cu
Au
Au
Au
Au
Au
Mn
Mn MnMn
Mn MnPb
ZnFl
FlFl
Cu
Fe
PbPb
AuGpMnMn
Mn
MnMnMn
Mn
MnPb
Au
CrCu
CuCu
Cu
Au
Pb
Gp
Gp
Gp
Gp
Au
Fe
Zn
FeFe
AuAu
FeFe
Fl
FeFe
Fe
Mn
CuCu
FeFe
Fe Fe
FeFe
Fe
FeFe
AuAu
Fe
Pb
Mn
Sn
CuCu
Cu
CuCu
Ta
Mn
Pb
AuAu
AuAu
Au
AuAu
Mn
Fe
Sd
FeFe
Mn
Mn
Mn
Fe
Mn
Mn
Au
Cor
Gvl
GvlGvl
Gvl
Gvl
GvlGvlGvl
Gvl
Brt
BrtPGEPGE
Brt
Cor
Brt
Brt
Dmd
BrlBrl
Clcp
Salt
Jasp
Cu, W
Shale
U, Cu
U, ZrU, Au
K2SO4
K2SO4Fe, Mn
Pb, ZnCu, PbAu, As
Au, Cu
Pb, Zn
Zn, Pb
Cu, Au
Cu, Au
Fe, MnMn, Fe
Cu, Pb
Pb, ZnCu, Zn
Zn, Cu
Pb, Cu
Au, Cu
Au, Cu
Au, Cu
Au, Cu
Fe, Mn
Cu, Co
Fe, Mn LnO, PbLnO, Pb
Cu, Au, V
U, Au, Pb
U, Cu, Pb
U, Pb, Cu
Au, Cu, As
Cu, Pb, Zn
Au, Cu, Co
Cu, Pb, As
Cu, Pb, Zn
Cu, Pb, Zn
Zn, Pb, Ag
Zn, Pb, Ag
Cu, Pb, ZnCu, Pb, Zn
Pb, Zn, Ag Au, Cu, Ag
K2SO4, Salt
Cu, U, Co, Mn
U, Pb, Zn, Cu
U, Au, Cu, Pb
Au, Cu, Zn, Pb
Cu, Zn, Pb, Au
Pb, Cu, Ce, LnOBrt, Sr, Mo, Ce
Cu, Au, Ni, PGE
U, Pb, Cu, Zn, Bi
Pb, Zn, Ag, Cu, U, Cd
Depth to unconformitymetres
High : 292.081
Low : -31.3929
0 10050 Kilometers
A large proportion of the A large proportion of the region remains underregion remains under--explored. AEM data can explored. AEM data can give more accurate depth give more accurate depth to target informationto target information
Geological interpretations from the Paterson AEM survey
AEM Signatures of Mineral Deposits
• Finally, a quick look at how the AEM performed over some of the mineral deposits in the area.
Geological interpretations from the Paterson AEM survey
Woodie Woodie plan & section
N
Geological interpretations from the Paterson AEM survey
m ASL
m ASL
FL 30850
FL 30860
Woodie Woodie plan & sectionPermian PatersonFm and/or Tertiary Oakover Fm
Permian or Tertiary valley fill
Woodie Woodie Mn depositsPalaeokarst with Mn ore
Jeerinah Fm
Geological interpretations from the Paterson AEM survey
Nifty plan & section
Permian (± Mesozoic)and Quaternary cover
Conductive Broadhurst FmBlack shale facies
Resistive Broadhurst Fmgreywacke facies
Resistive Broadhurst Fmgreywacke facies
Permian and Quaternary cover
Geological interpretations from the Paterson AEM survey
Telfer plan & section
Conductive unit inTelfer Member Permian and Quaternary coverPermian and Quaternary cover
Geological interpretations from the Paterson AEM survey
Conclusion
• Regional AEM data give us:– A better understanding of paleotopography;– A better information on under-cover extent of
mineralised rocks including 3-D disposition;– Reduced risk by providing more accurate
depth to target information;– Much more information on landscape