Testing the UNCOVER paradigm:
Crustal fluid pathways in the Curnamona ProvinceGraham Heinson and Ben Kay
University of Adelaide Electrical Earth Imaging group
Institute for Mineral and Energy Resources
(Begg, 2015) (McCuaig & Hronsky, 2014)
Regional-to-Camp Scale: AusLAMP
Robertson et al. (2016)
Resistivity depth slices from AusLAMP
long period MT data
C2 C1
Modified from Fabris et al. (2010)
DTB (m) Min. Occ.
Camp-to-Deposit Scale: Broadband MT
Scale-reduction
AusLAMP SectionBBMT Section
C3
C4
C4
C3
C1 C1
C2
C3
C4
C1
R1 R1R1
C2
Regional – Camp – Deposit Scale
C3
C4
C1
R1 R1R1
C2
Regional – Camp – Deposit Scale
C3
C4
C1
R1 R1R1
C2
Camp – Deposit Scale
Deposit Scale
Conductivity (S/m)
LNM 10 1 Yalkalpo 1 Yalkalpo 2
LNM 10 1 17 km S
Yalkalpo 1 8.4 km N
Yalkalpo 2 12 km N
FROME AEM#2000101
C1
R1R1
C2
C1
N S
W E
0 km 100 km
0 km 100 km
0 km
20 km
0 km
20 km
North-south MT profile
08GA-C1
C2C3
C4
C1
Olympic Dam Line
Curnamona Line
R1 R1
0
5
10
15
20
100 km
C2C3
C4
C1R1 R1
0
5
10
15
20
100 km
Conclusion
Long-P
eriod M
T
Bro
adband M
T
Portia
Kalkaroo
Goran Boran
Kate Robertson
Yohannes Didana
Stephan Thiel
Samuel Jennings
Paul Soeffky
Acknowledgments
